[HN Gopher] Ice core scientists in East Greenland reach bedrock
___________________________________________________________________
 
Ice core scientists in East Greenland reach bedrock
 
Author : giuliomagnifico
Score  : 405 points
Date   : 2023-07-31 16:22 UTC (6 hours ago)
 
web link (news.ku.dk)
w3m dump (news.ku.dk)
 
| deafpolygon wrote:
| Isn't this the basically the plot to the prequel of The Thing?
 
| taf2 wrote:
| From the picture that looks like a pretty large hole... any
| chance that execrates the melting process by increasing the
| surface area? Or is it insignificant just curious if someone has
| thought about or done any calculations...
 
| sgirard wrote:
| Interesting: "Towards the base, the ice is more than 120,000
| years old and dates back to the last interglacial period, a time
| when the atmospheric temperature above Greenland was 5degC warmer
| than today."
 
  | [deleted]
 
  | thomasahle wrote:
  | See also this timeline of the last four inter-glacial periods:
  | https://co2coalition.org/wp-content/uploads/2021/09/104-4000...
  | 
  | It also shows how crazy it would be if we get the projected 2-3
  | degrees average temperature increase. Even in a period where
  | we'd expect to be going into a new ice age; instead shooting to
  | a previously unseen high temperature.
 
    | slashdev wrote:
    | On the other hand if we only have 2-3 degrees of warming, if
    | that's enough to prevent the next ice age, didn't we just
    | dodge a massive icy bullet? Might we not one day thank
    | ourselves for doing something reckless and stupid that
    | actually worked out?
    | 
    | Yeah a warmer climate brings all kinds of horrible changes.
    | But food still grows in the northern hemisphere. A colder
    | climate is arguably even worse for us.
    | 
    | By the way, that's no excuse to keep doing what we're doing.
    | Limiting warning at 2-3 degrees will be nice. Things get
    | really horrific above 4. At some unknown point feedback
    | cycles really kick in and we go to 5-10 degrees and get
    | completely fucked. We really have to not find out where that
    | threshold is.
 
      | kuprel wrote:
      | I didn't realize that the vast majority of the time Earth
      | is in an ice age. What causes it periodically like this?
 
        | slashdev wrote:
        | It's mostly caused by Milankovitch cycles. Which are
        | cyclic variations in our orbit around the sun.
        | 
        | The earth varies in distance to the sun and axial tilt
        | and precession. Like waves, there factors can either
        | overlap and somewhat cancel or they can stack for a
        | larger effect.
 
        | autokad wrote:
        | ice ages didn't happen until after the asteroid strike.
        | Antarctica moving into the south pole is likely a large
        | part of it, but they don't really understand ice ages
        | that well TBO. Anyhoo, the Earth was a lot warmer prior
        | to the strike and we have been going through extinction
        | events every 100k years.
 
        | mkl wrote:
        | By "the" asteroid strike I'm guessing you mean the one
        | 66M years ago? There were definitely ice ages before
        | that, likely including one or more Snowball Earth phases
        | (the whole surface frozen):
        | https://en.wikipedia.org/wiki/Snowball_Earth.
 
  | monero-xmr wrote:
  | [flagged]
 
    | barbazoo wrote:
    | Please correct me if I'm wrong. The amplitudes of co2 ppm
    | seem to always have been within a certain band though,
    | topping out at 300ppm. Right now, we're at 420ppm and
    | increasing what looks like exponentially. [0]
    | 
    | I'm not saying humans won't be fine but we've never been so
    | dependent on the stability of the climate before. People will
    | die, get displaced, suffer economically, etc as far as I
    | understand.
    | 
    | [0] https://www.climate.gov/news-features/understanding-
    | climate/...
 
      | foota wrote:
      | I don't think 800,000 years is that long on the geological
      | time scale. (Not that I don't think global warming is a big
      | deal etc etc)
 
        | barbazoo wrote:
        | It's not but it's also not much less time than what we
        | consider "humans" to have been around and we're talking
        | about co2 in the atmosphere in the context of whether
        | humans will be fine or not.
        | 
        | Of course, for earth it doesn't matter at all.
 
      | px43 wrote:
      | It was over 4000ppm during the Cambrian period 500m years
      | ago, then down to about where it is today in the
      | Carboniferious period, during the 60 million year period
      | where trees evolved to make wood, but nothing had evolved
      | to eat it yet, so dead trees literally just piled up for 60
      | million years. Then during the Mezozoic it went up into the
      | 2000s again, lots of dino farts or something? Then back
      | under 1000 again and dropping until the last 100 years or
      | so.
      | 
      | https://en.wikipedia.org/wiki/Carbon_dioxide_in_Earth%27s_a
      | t...
      | 
      | Of course, there were also mass migrations and extinctions
      | as the environment changed so radically, which seems like
      | something that would be nice to avoid.
 
        | barbazoo wrote:
        | I was just responding to parent who said
        | 
        | > On the positive, the earth has been much warmer and
        | much colder, and has had more carbon and less carbon in
        | the atmosphere.
        | 
        | the way I read it suggesting that it'll be fine. But it
        | won't be, if co2 increased to 4000 ppm quickly enough,
        | humans would not be fine. There were no humans during the
        | time you were describing.
 
    | petemir wrote:
    | Part of the problem, which you fail to address, is the time
    | frame when these changes take place and the possibility of
    | the ecosystem to adapt. Yes, we've been much cooler and much
    | warmer, with these changes taking place over thousand of
    | years: not a couple of centuries.
 
    | [deleted]
 
    | nextaccountic wrote:
    | Quick changes in climate generally lead to extinction events.
    | And indeed we are in the middle of one. And it's caused by us
    | 
    | https://en.wikipedia.org/wiki/Holocene_extinction
    | 
    | Life will go on. Humans? Maybe. Human civilization will be
    | disrupted for sure
    | 
    | Also: here's a visualization of how fast the climate changed
    | in the last 20000 years vs today
    | 
    | https://xkcd.com/1732/
    | 
    | The short term effects are all about the slope. And the short
    | term is all that matter to us, because if we don't pass
    | through this bottleneck we won't have a long term (it may
    | well be our "great filter" preventing us from spreading
    | through the stars)
 
    | sleet_spotter wrote:
    | A critical piece is the speed at which the climate is
    | warming. The Earth has had much warmer and colder periods in
    | its history that (most) life adapted to. However, life was
    | only able to adapt happened because those changes happened at
    | a sufficiently slow pace. To perhaps put the current trend in
    | the context of geologic time, there have been 5 mass
    | extinctions in the fossil record of life on Earth. These are
    | associated with rapid changes in climate (e.g. asteroid
    | impacts, large volcanic eruptions). Anthropogenic climate
    | change is driving Earth's 6th mass extinction event. To be
    | clear: what is happening now has not happened often in
    | Earth's history. Life has survived, but it has not been
    | pretty. Some alarmism is warranted from the ecosystem
    | collapse alone.
    | 
    | https://en.wikipedia.org/wiki/Extinction_event
    | https://en.wikipedia.org/wiki/Holocene_extinction
 
    | btilly wrote:
    | More at issue is that rates of change matter.
    | 
    | When temperature rises slowly, ecosystems adapt in parallel
    | to the change. When temperature rises fast, ecosystems don't.
    | And so we have major die-offs of coral and trees, without
    | corresponding colonization in places where they could now
    | live.
    | 
    | When CO2 rises slowly, the ocean's pH is buffered by large
    | deposits of calcium carbonate on the bottom. When CO2 rises
    | fast, we get ocean acidification, which is on track to be the
    | most extreme shellfish extinction event in the last 50
    | million years.
    | 
    | Therefore larger absolute past climate changes were less
    | likely to have extreme impacts than faster present climate
    | changes.
 
    | alberth wrote:
    | > _" On the positive, the earth has been much warmer and much
    | colder"_
    | 
    | The concern is, during these hotter/colder periods of earth's
    | existence - what happened to life on earth during that time?
    | 
    | Did populations decline? Was life nearly run into extinction
    | (dinosaurs, etc)?
 
    | bparsons wrote:
    | My whole country being on fire since May has been pretty
    | apocalyptic.
 
    | spockz wrote:
    | Although indeed the temperatures and GHG have been lower and
    | higher on Earth before, that was never with the amount of
    | humans we have now. Our economy and society is quite
    | optimised and our infrastructure hubs are largely located on
    | coasts. Our prosperity also relies on a large amount of
    | sophisticated technology that is hard to replace and to
    | bootstrap.
    | 
    | So although the human species will probably survive a drastic
    | climate change, many individuals will not due to famine, lack
    | of medical supplies and care, and war over the remaining
    | resources.
 
    | hnhg wrote:
    | It is also because it will result in incredible levels of
    | migration and competition for resources in the short term (ie
    | wars). Yes, humanity will survive but it might make global
    | shocks like the pandemic seem very tepid by comparison.
 
    | shostack wrote:
    | The earth may have survived those changes, but not all its
    | inhabitants may have. So there definitely is still reason to
    | worry as far as humanity is concerned.
    | 
    | The major ecological shifts may bring change humanity does
    | not bounce back from.
 
      | notfish wrote:
      | When the cause for optimism is "some humans will probably
      | survive", I don't feel very optimistic
 
    | FrustratedMonky wrote:
    | >>"The doomsday cult saying we are all going to die, or that
    | every single heat wave and natural disaster can be pinned on
    | extra carbon, are just yet another in a long line of
    | apocalyptic predictors"
    | 
    | The problem with this argument is that 'humans' surviving, is
    | different than 'our nice comfortable human society'
    | surviving.
    | 
    | Yes, the human species as an animal that can survive by
    | foraging, probably will survive. That isn't a great argument.
 
    | dakial1 wrote:
    | Not all natural disasters can be pinned into global warming
    | (earthquakes for example), also some weather related
    | disasters are caused by cyclical patterns (e.g. El Nino), but
    | certainly the higher frequency (and potency) of some weather
    | related disasters are already linked to human influence:
    | https://news.un.org/en/story/2021/09/1098662
    | 
    | Is not doomsday as the world won't change overnight, but some
    | areas of the globe will suffer a lot from the higher
    | intensity of the weather and this will probably create a lot
    | of global challenges and might bring (mostly) overcome
    | tragedies, like widespread famine, back to the news
 
    | mariuolo wrote:
    | It's true the Earth has been much warmer and much colder, but
    | it's also true we haven't always been there.
 
    | anigbrowl wrote:
    | _The doomsday cult_
    | 
    | Oh shut it. You can't have any knowledge at all about this
    | issue and not appreciate that the problem is not temperature
    | as such but the rapidity of the change - over 150 years
    | rather than 15000. Your troll post is an insult to
    | intelligence.
    | 
    | Folks, don't waste your time trying to reason with such bad-
    | faith arguments. It's a form of theft, because the time cost
    | to refute bullshit is about 10x that to spew bullshit. And
    | the above post is just that - bullshit.
    | 
    | Before someone invokes the HN guidelines and talks about
    | curious conversation, recognize that throwing phrases like
    | 'doomsday cult' into a discussion of a serious scientific
    | project that has hit a milestone after many years of effort
    | has only one purpose, and that is to derail. Flagging and
    | downvoting are all very well, but there are also times when
    | it's necessary to call bullshit.
 
      | briantakita wrote:
      | You seem angry, so I'm going to try to explain (from my
      | perspective) why someone may have the perception that you
      | reacted to.
      | 
      | There is plenty of criticism over relying on mathematical
      | models that fail to accurately predict the future (all of
      | the glaciers were predicted to have melted 3 years ago,
      | snow was supposed to have been a thing of the past, etc.),
      | cherry picking data, questionable measurement & sampling,
      | not considering other forcing inputs, etc. It's a
      | complicated claim that has valid criticism on it's
      | foundational pieces If any foundational premise of the
      | claim is invalidated, the entire model is invalidated. The
      | consensus models are complicated so I'm not surprised that
      | it has a difficult time standing up against scrutiny &
      | needs to be adjusted frequently.
      | 
      | There is also dissent among scientists, including from
      | Nobel Laureates (who had opportunities cancelled after
      | dissenting). "The doomsday cult" reference comes from the
      | doom & gloom sensationalism. For example, I a heard chorus
      | of "we are fucked" from coworkers in the office about 15
      | years ago in response to some news back then. I don't agree
      | that "we are fucked". Humans have been through more
      | environmentally challenging times with less technology &
      | global knowledge.
      | 
      | The climate is changing...always has changed & always will
      | change. What are we going to do about it? Are we going to
      | pretend that we can stave off the inevitable,
      | taxing/restricting the population which weakens their
      | ability to adjust to these inevitable changes...while
      | wealth is concentrated to the elites? There is a widespread
      | perception that is happening. When the issues reach it's
      | crescendo later in this decade & the fallout in the 2030s
      | (winter occurs after the Solar Solstice, solar exposure
      | increases during winter), there will be many who will not
      | buy the APGW narrative as the reason for their problems.
      | The peaceful solution is a decoupling from systems that
      | don't benefit the person/group, which I expect to happen.
      | Others, such as Peter Turchin think there is a high
      | probability of violent uprising & he seems to think
      | addressing APGW is a unifying force...I disagree on both
      | premises but I think his analysis is valid & worth getting
      | into.
      | 
      | I think the animus generated by climate alarmism putting
      | the blame on the population reduces effective cooperation
      | among people & will be exasperated as the climate does
      | change, as the Geomagnetic wander deepens in it's cycle, as
      | magnetic fields fluctuate in our solar system, etc. A
      | spirit of cooperation will unify humanity while the blame
      | game will cause conflict. Doom & gloom is unhelpful. The
      | "doomsday cult" will increase in their doom & gloom as
      | people walk away from their petulance & their social
      | leverage wanes.
 
        | arp242 wrote:
        | > all of the glaciers were predicted to have melted 3
        | years ago
        | 
        | I don't think any mainstream models predicted that? Which
        | model was that?
        | 
        | Also remember that our actions are influenced by models.
        | "If current trends persist, then in 20 years [...]" may
        | very well be true, but if we take action based on those
        | predictions (e.g. change the trend) then the outcome will
        | be different.
        | 
        | You can see this clearly in population levels of things
        | like elephants[1] or whales[2]: people who were
        | predicting the extinction of whales and elephants weren't
        | wrong.
        | 
        | [1]: https://ourworldindata.org/grapher/african-elephants
        | 
        | [2]: https://www.researchgate.net/figure/General-
        | estimated-popula...
 
    | toss1 wrote:
    | Yes, there have been warm and cold intervals in the past.
    | 
    | NONE of them happened at anything approaching the _RATE_ of
    | today 's anthropogenic warming.
    | 
    | Our climate is warming literally orders of magnitude faster
    | than any previous change. This is overwhelming the ability of
    | ecosystems to adapt.
    | 
    | Moreover, this is entirely preventable -- we're doing it, we
    | can stop it.
 
    | snowwrestler wrote:
    | People worry about accelerating climate change now because we
    | live here now.
    | 
    | It's not a theoretical science thing. We have farms and
    | cities and towns and bridges and dams and reservoirs in
    | particular places, and we are accelerating the depreciation
    | of many of them. The result will be tremendous loss of
    | wealth, movement of populations, and the associated social
    | consequences of those.
    | 
    | Humanity doesn't hate itself, we like ourselves, which is why
    | we are so concerned about what we are doing to ourselves.
 
      | viscanti wrote:
      | > Humanity doesn't hate itself, we like ourselves, which is
      | why we are so concerned about what we are doing to
      | ourselves.
      | 
      | Yeah. The argument that single cellular life or some small
      | animals might survive and eventually evolve into something
      | else is a bit weird for people who are hoping they don't
      | die out like many species have in the past when there have
      | been major changes to climate and carbon levels.
 
        | warning26 wrote:
        | Exactly. People often get lost in this "we must save the
        | planet" argument, but realistically, the planet is gonna
        | be fine.
        | 
        | Preventing climate change is about saving _humanity_ ,
        | not the planet.
 
        | etrautmann wrote:
        | How is this pedantic point useful in any way?
 
        | mikestew wrote:
        | I swear, if _one_ more person quotes an old George Carlin
        | bit, as if it were still clever or useful...or as if said
        | person didn 't know what was meant by the statement.
 
        | xp84 wrote:
        | > How is this pedantic point useful in any way?
        | 
        | Because it forces us to recognize that the risk isn't to
        | "the Earth" as a separate entity, but to ourselves
        | specifically (well, our future descendants).
        | 
        | We've already confirmed through our behavior that humans
        | largely don't care about any other part of the Earth
        | ecosystem, so asking people to basically do the right
        | thing as a favor to the Earth are probably wasting their
        | time.
 
      | toshk wrote:
      | Yeah but there is more to it. There are active crisis, like
      | cancer & heart disease. Or upcoming ones like Alzeimer &
      | Parkinson. That in the current day already affect more
      | people per year, then the climate crisis will affect in the
      | worst prognoses in a 100 years*.
      | 
      | But Climate change is different, it speaks to the psyche of
      | humans, the modern story of the flood. And in the same way
      | it gives people meaning & without religion in the West they
      | form morality around it. Those for it, are good, those
      | against it, are bad.
      | 
      | That doesn't mean its not something important or real, and
      | we have to solve it. But it's one of the many things for us
      | humans to solve.
      | 
      | *In worst prognoses, climate changes will affect 10 mil
      | deaths per year, which is the same amount cancer is doing
      | every year today.
 
        | cycomanic wrote:
        | Except that neither of the things you mention affects
        | more people than climate change will. The estimate is
        | that there are about 54 M people World wide suffering
        | from alzheimer.
        | 
        | The worst case projection for 2100 for just sea rise is
        | 4-5m on global average (but much higher in some areas) ht
        | tps://iopscience.iop.org/article/10.1088/1748-9326/acb504
        | 
        | To put that into perspective the average altitude of
        | Bangladesh is 9m above sea level, but the majority of the
        | population lives in he south at about 0-1m of altitude.
        | So there would just in Bangladesh alone be more people
        | (let's say 50% of 160M) directly affected by climate
        | change than alzheimer world wide. We are not even talking
        | about the indirect effects of displacing 60M people, all
        | the other countries and all the other effects of climate
        | change.
        | 
        | Apart from that, the argument is under the false premise
        | that we shouldnt do anything anyway because there is
        | worse things. By that argument we should also not do
        | something about alzheimer, because more people die of
        | cancer.
        | 
        | So I question what your aim was with your argument. It
        | was clearly using wrong facts and was under a false
        | premise.
 
        | toshk wrote:
        | Just because they will below sea level doesn't mean they
        | will all die. That's a bit ludicrous. Even more ludicrous
        | are your nrs 4-5 meters, will get to that.
        | 
        | Whole of Holland is below sea level at the moment. Yet we
        | are miraculously sitil alive.
        | 
        | To take it further, in a 100 years every house in Holland
        | that's here now will still be standing.
        | 
        | Now certain countries don't have the skills that the
        | Dutch have, and we should help them. But this isn't
        | something that will come unexpected, so we have the time
        | to do so. Half of Dubai was created out of the sea.
        | 
        | But, even then 4-5 meters is too much. Worst case is less
        | then 1m. Till now we got 20cm. Expectance by Dutch gov.
        | is this between another 20 and 86 cm in the next century:
        | https://www.knmi.nl/kennis-en-
        | datacentrum/uitleg/zeespiegels...
        | 
        | Back to the medical argument. Even if parts are flooded,
        | which is terrible. Moving away is not the same as not
        | being able to use your brain or dying.
 
    | downWidOutaFite wrote:
    | If you're in the "head in the sand cult" you might be
    | obliviously happier than the the "doomsday cult", but our
    | ancestors will hate you much more.
 
  | mytailorisrich wrote:
  | Iirc, the CO2 concentration now as been pumped up higher than
  | it was then, which is in part what is worrying because temps
  | might then potentially shoot even higher.
  | 
  | Bottom line: we need large scale carbon capture quickly because
  | even if we reach net zero CO2 will take millenia to drop back
  | to the level it was pre-industrial revolution.
  | 
  | Edit: I wouldn't focus on "pre-industrial levels" specifically,
  | the point is that there is too much now so we most likely want
  | concentration to drop as soon as possible.
 
    | lehi wrote:
    | The Keeling Curve is eye-opening for understanding our
    | current versus (pre-)historical CO2 levels:
    | https://tywkiwdbi.blogspot.com/2023/07/introducing-
    | keeling-c...
 
    | BurningFrog wrote:
    | > _Bottom line: we need large scale carbon capture quickly_
    | 
    | The short term solution/bandaid is pumping SO2 into the
    | stratosphere while we figure out carbon capture.
 
      | XorNot wrote:
      | I do wonder if some of the "massed solar sail" ideas for
      | terraforming Mars' atmosphere would work here (in short:
      | use cellphone processors to build and launch a couple
      | hundred thousand solar-sail equipped satellites).
      | 
      | Because it would be expensive, but it would kill several
      | birds with one stone: we (1) prove whether the concept
      | would work on Mars, (2) develop the technology to do it,
      | and (3) unlike SO2 in the atmosphere, "switching it off" or
      | modifying the scale of the effect can be done almost
      | instantly (you could remove the swarm by having it fall
      | back to an Earth orbit).
 
    | elzbardico wrote:
    | Why do we need to get back to the levels pre-industrial
    | revolution?
 
      | angiosperm wrote:
      | We have also pumped a very large amount of long-lived
      | fluorine compounds into the air, that will last for
      | centuries. They have from 2500x to 25000x times the
      | "greenhouse gas warming potential", kg for kg. They are
      | mostly refrigerants (CFCs, HFCs, and soon their successors)
      | and transformer insulation gas (SF6). Volcanoes do emit
      | some amount of fluorine compounds, too.
      | 
      | We also have a great deal of methane leakage, which is
      | usually cited as 25-100x, and we may soon have a lot of
      | hydrogen leakage, at >100x. Rocket launches are installing
      | water vapor, another one, into the stratosphere like never
      | before.
      | 
      | So even if we got CO2 down to a pre-industrial level, we
      | would still have heat forcing from the fluorine- and other
      | compounds.
      | 
      | Capturing CO2 is kind of pointless until we get emissions
      | under control. I.e., a dollar spent preventing emissions
      | buys much more than a dollar spent capturing. Solar panels
      | and wind turbines directly displace mass emitters of CO2.
 
        | specialist wrote:
        | Yes and: I understand that we want to prevent the non-
        | human emissions from becoming a positive feedback loop.
        | Meaning that at some tipping point, the thawing tundra,
        | burning forests, and acidic oceans will continue to get
        | worse, even if/when human emissions completely stop.
 
        | mytailorisrich wrote:
        | I don't know about all compounds but CFCs stay in
        | atmosphere for about a century only and we've already
        | banned them, and methane has a very short lifetime of
        | about 12 years. So we 'only' need to control emissions of
        | those to solve the problem.
        | 
        | On the other hand, as said, CO2 stays for centuries if
        | not 1,000+ years so at this point net zero is only half
        | the job though probably the hardest part.
 
        | zdragnar wrote:
        | Methane, at least, breaks down to CO2, no?
 
      | e_i_pi_2 wrote:
      | That is the point where we started adding greenhouse gases
      | that lock in energy from the sun, we need to at least get
      | back to those levels to start releasing some of the heat.
      | Otherwise we're containing to add insulation to an oven
      | that already overheating - you'd ideally want to take off
      | all the insulation and the metal casing since you can't
      | turn off the heat, but the casing isn't an option so we
      | need to remove the insulation and hope it hasn't gotten too
      | bad yet
 
      | mytailorisrich wrote:
      | The point is that net zero is most likely not going to stop
      | warming with 400+ppm CO2 in the atmosphere. CO2
      | concentration most likely has to drop but naturally it does
      | so very slowly. Arguably at this point we already need
      | _cooling_ because 40+C every summer in half of Europe (for
      | instance) is getting annoying...
 
        | gottorf wrote:
        | > at this point we already need cooling
        | 
        | A colossal volcanic eruption could do the trick, and
        | those seem to happen rather unnervingly frequently.
 
      | sleet_spotter wrote:
      | Pre-industrial CO2 concentration is synonymous with the
      | "natural concentration", at least in the recent past. We
      | made a very large change that has thrown Earth's systems
      | out of equilibrium. Returning to pre-industrial CO2 levels
      | would undo that change and bring things back towards
      | equilibrium.
 
        | thrashh wrote:
        | Like the other reply said, there is no natural
        | equilibrium.
        | 
        | We want to return to pre-industrial levels because we're
        | used to it and we liked it more then.
 
        | tenpies wrote:
        | I like to think of it as scrappy terraforming because we
        | aren't even sure we could handle any of the naturally
        | occurring variation.
        | 
        | Scrappy because, well the planet doesn't quite become
        | uninhabitable and we're starting from the end-game.
        | Science fiction also had me expecting some very cool
        | terraforming infrastructure, not psy-ops to get the serfs
        | to eat bugs.
 
        | thrawa8387336 wrote:
        | Really
 
        | nonethewiser wrote:
        | "Natural concentration" is not the right way to look at
        | it because there are higher concentrations that predate
        | the industrial revolution and humans. The all time high
        | (that we know of) is from about 350,000 years ago. This
        | was by all means natural and pre industrial revolution.
 
        | adhesive_wombat wrote:
        | "The only known natural concentration empirically
        | compatible with long-term human civilisation".
        | 
        | "The planet did exist/will exist just fine without us" is
        | a pretty worn truism. You might as well wryly note that
        | water isn't natural because everything was hydrogen once.
 
        | gottorf wrote:
        | > empirically compatible with long-term human
        | civilisation
        | 
        | Empirically observed, atmospheric CO2 went from ~320ppm
        | to ~410ppm from 1970 to 2020[0], during which period the
        | human population more than doubled from ~3.7B to ~7.8B
        | and yet deaths caused by climate dropped threefold[1]
        | (not 1/3 the rate; 1/3 in absolute number).
        | 
        | [0]: https://www.climate.gov/news-features/understanding-
        | climate/...
        | 
        | [1]: https://library.wmo.int/doc_num.php?explnum_id=10989
 
        | adhesive_wombat wrote:
        | On the scale of human civilisation, 50 years is hardly
        | "long term".
        | 
        | Polonium by that ultra-short-relative-term reckoning is
        | not only harmless as it you still feel fine 10 minutes
        | later, but actually healthsome as you rather feel
        | refreshed by the delicious green tea you just drank in
        | that 5-star hotel bar.
 
        | colechristensen wrote:
        | They are dynamical systems, there is no equilibrium. See
        | also: climate charts for the last few ice age cycles.[1]
        | In the bigger picture we _want_ to modify Earth 's
        | climate and definitely do not want to end the current
        | interglacial period, to be fair we've already done that,
        | but returning to a "natural" pre-human climate cycle on
        | the 10,000 year scale is not desirable.
        | 
        | 1.
        | https://energyeducation.ca/wiki/images/8/8f/Ice_ages2.gif
 
        | pinkmuffinere wrote:
        | Dynamical systems can have equilibrium points --- e.g. an
        | inverted pendulum is stable when hanging straight down.
        | If you deviate too far from an equilibrium point, the
        | system may find another equilibrium that is less
        | desirable for the user. I'm not an expert in climate
        | change, but those things certainly happen for engines,
        | robots, and other systems.
 
  | adolph wrote:
  | 120k years ago in context:                 * 170,000 years ago:
  | humans are wearing clothing by this date.       * 125,000 years
  | ago: the peak of the Eemian interglacial period.       *
  | ~120,000 years ago: possibly the earliest evidence of use of
  | symbols etched onto bone       * 75,000 years ago: Toba Volcano
  | supereruption that may have contributed to human populations
  | being lowered to about 15,000 people
  | 
  | https://en.wikipedia.org/wiki/Timeline_of_prehistory
  | 
  |  _The Eemian climate is believed to have been warmer than the
  | current Holocene. Changes in the Earth 's orbital parameters
  | from today (greater obliquity and eccentricity, and
  | perihelion), known as Milankovitch cycles, probably led to
  | greater seasonal temperature variations in the Northern
  | Hemisphere. During the northern summer, temperatures in the
  | Arctic region were about 2-4 degC higher than in 2011._
  | 
  |  _The hippopotamus was distributed as far north as the rivers
  | Rhine and Thames. . . . The prairie-forest boundary in the
  | Great Plains of the United States lay further west near
  | Lubbock, Texas, whereas the current boundary is near Dallas. .
  | . . Sea level at peak was probably 6 to 9 metres (20 to 30
  | feet) higher than today . . . ._
  | 
  | https://en.wikipedia.org/wiki/Eemian
 
    | orangepurple wrote:
    | This raises a very critical point. Nuclear is the only
    | dependable energy source. Fossil fuels will run out or go out
    | of favor. Solar and wind on the other hand will become
    | victims of the next major volcanic eruption as ash destroys
    | them or renders them ineffective.
 
      | dredmorbius wrote:
      | An eruption significant enough to impact solar and wind
      | generation globally will also affect _other_ critical
      | requirements of humanity, and the Earth 's ecosystem,
      | globally.
      | 
      | Which is to say: You Will Be Having Bigger Problems.
      | 
      | Recovery from regional meterological catastrophes is well
      | within human capabilities.
 
      | ricardobeat wrote:
      | Nuclear facilities seem pretty fragile / demanding, I doubt
      | one would survive any kind of apocalyptic event. The
      | infrastructure supporting it will be gone.
 
        | fullstackchris wrote:
        | isnt that the case with any advanced technology?
        | (including wind and solar)
 
      | XorNot wrote:
      | Deep drilling based geothermal can fill this role too
      | though - and does have the substantial benefit over nuclear
      | that it leaves no surface-supply chains for resources
      | (uranium).
      | 
      | Given that we're so close to being able to do it, we
      | honestly need a Manhattan project initiative to push it
      | through to reality (with the outcome being the machine and
      | process to do the drilling).
 
    | angiosperm wrote:
    | There is definite evidence of hominins in North America
    | 130,000 years ago (search "Cerutti mastodon"). Nobody knows
    | if they were _H. erectus_ , Neanderthal, Denisovan, modern
    | humans, or "other", but with an interglacial at 125,000 years
    | ago, it is not hard to see how they could have got here.
 
      | biztos wrote:
      | Wikipedia suggests this is not definitive, and maybe not
      | even evidence:
      | 
      | https://en.wikipedia.org/wiki/Cerutti_Mastodon_site#Critici
      | s...
      | 
      | This article is much more sympathetic (and also a fun
      | read):
      | 
      | https://www.latimes.com/local/california/la-me-cerutti-
      | masto...
      | 
      | I'm no expert but it seems like this is still a
      | controversial idea.
 
    | wheelerof4te wrote:
    | "75,000 years ago: Toba Volcano supereruption that may have
    | contributed to human populations being lowered to about
    | 15,000 people."
    | 
    | The key question is: How much CO2 did that super-eruption
    | emit into the atmosphere?
    | 
    | In our hurry to attribute climate change to our meager impact
    | on this planet, we tend to forget what horrors an eruption of
    | this magnitude can cause. And who knows how many of them
    | happened during the past millennia.
 
      | pmayrgundter wrote:
      | The figure I've found is 2800 km^3 of approximately
      | granite, which at 2.7 tonnes per cubic meter gives about a
      | billion gigatons ejecta.
      | 
      | I've never found a CO2 estimate, but did find that it's a
      | significant amount of that mass, as is SO2.
      | 
      | It wasn't worth me doing more of a sketch since it's not
      | clear how to model the effects of such a massive system.
      | 
      | I was struck tho, that the magnitude of this and a few
      | other events in the not too distant past, are vastly larger
      | than even all put nuclear war
      | 
      | It's not clear to me that our CO2 emissions are very
      | significant in comparison
 
        | dredmorbius wrote:
        | Wikipedia cites a range of 2,000 -- 13,000 km^3.
        | 
        | 
        | 
        | I'm _not_ finding a good source on overall composition of
        | volcanic eruptions, either generally or by type. Anyone
        | else?
        | 
        | One of the largest volcanic events I'm aware of is the
        | Siberian Traps eruption, about 250 mya, with a volume of
        | about 4 million km^3, another three orders of magnitude
        | greater than Tomba.
        | 
        | This has been linked to the Permian-Triassic mass
        | extinction event, with the mechanism being release of
        | methane clathrates and/or stimulating growth of a microbe
        | which released vast quantities of methane into the
        | atmosphere, killing ~81% of all extant marine species and
        | 70% of terrestrial vertebrate species.
        | 
        | 
        | 
        | "The level of atmospheric carbon dioxide rose from around
        | 400 ppm to 2,500 ppm with approximately 3,900 to 12,000
        | gigatonnes of carbon being added to the ocean-atmosphere
        | system during this period."
        | 
        | -- Wikipedia, citing Wu, Yuyang; Chu, Daoliang; Tong,
        | Jinnan; Song, Haijun; Dal Corso, Jacopo; Wignall, Paul
        | B.; Song, Huyue; Du, Yong; Cui, Ying (9 April 2021).
        | "Six-fold increase of atmospheric pCO2 during the
        | Permian-Triassic mass extinction". Nature Communications.
        | 12 (1): 2137. Bibcode:2021NatCo..12.2137W.
        | doi:10.1038/s41467-021-22298-7.
        | 
        | 
 
      | mschuster91 wrote:
      | > And who knows how many of them happened during the past
      | millennia.
      | 
      | We at least have a significantly large list of what we know
      | [1] - that's part of the purpose of core drilling, the ash
      | deposits worldwide can be linked together to estimate where
      | ash traveled to. Also, craters and their surrounding can be
      | drilled into to determine eruption events.
      | 
      | [1] https://en.wikipedia.org/wiki/List_of_large_volcanic_er
      | uptio...
 
        | pmayrgundter wrote:
        | Here's a study:
        | 
        | The size and frequency of the largest explosive eruptions
        | on Earth, Mason 2004
        | 
        | https://www.researchgate.net/publication/227000709_The_si
        | ze_...
 
      | FireBeyond wrote:
      | I think people struggle with the magnitude.
      | 
      | Mt St Helens, for example. Not the largest eruption.
      | 
      | But a landslide of approximately 2.5km^3 (over 3 billion
      | cubic yards).
      | 
      | Okay, some say, so that is a lot of earth...
      | 
      | and then you learn that the landslide was moving at speeds
      | of up to 160mph.
      | 
      | That's a LOT of energy.
 
      | staunton wrote:
      | Volcanoes aren't about the CO2, they're about the ash which
      | blocks out the sun and makes it colder.
 
  | newfonewhodis wrote:
  | I'm not a scientist so I'm curious why this is interesting.
 
    | p1esk wrote:
    | Presumably because we can find well preserved organisms from
    | that time.
 
    | snowwrestler wrote:
    | I think people who are not already familiar with the known
    | history of the Earth find it interesting that there have been
    | higher CO2 levels and temps than there are now.
    | 
    | And I agree: the history of the Earth _is_ interesting. Which
    | is why so many people study and work in the field of geology.
 
    | sgirard wrote:
    | I find it interesting because it raises questions that I
    | don't have answers to. For example:
    | 
    | - What caused the temperature above Greenland to be 5degC
    | warmer than today? Why is it cooler now compared to 120,000
    | years ago? What causes the interglacial periods? Is
    | glaciation the more common state of the climate?
    | 
    | - The article says the ice sheet is melting at the bottom?
    | Why? Pressure from above? Friction from movement? Heat from
    | the Earth? Something else?
    | 
    | - Was the ice sheet shrinking or growing when the
    | temperatures above Greenland were 5degC warmer than now? Does
    | existence of the ice sheet imply that 5degC warmer for some
    | period of time is not enough to melt the Greenland ice sheet?
    | 
    | - How much climate data has been lost to melting from the
    | bottom? Is the ice sheet thickening or thinning compared
    | 120,000 years ago? How would we know?
    | 
    | - How much has the Greenland land mass moved in 120,000 years
    | due to plate tectonics? Could this have impacted the ice
    | sheet in this short amount of time?
    | 
    | - Humans adapt. How did humans adapt to a climate that was
    | warmer by up to 5degC 120,000 years ago?
    | 
    | - How long did the warm temperatures persist 120,000 years
    | ago? 10,000 years? 50,000 years? Or more?
    | 
    | - Could a cooling climate be more worrisome to humanity than
    | a warming one?
 
    | detourdog wrote:
    | It's interesting because the whole ice cap as we know it is
    | around 120k years ago which I don't consider the long ago on
    | human development scale. This also appears to mean that in
    | the past 120K there wasn't a polar ice cap. I read that as
    | the worst case scenario we should be using for long term
    | planning. This also may help determine how fast the ice was
    | built and how fast it will melt.
    | 
    | I'm completely an armchair ponderer.
 
      | lumost wrote:
      | This will also assuredly fuel some interesting ideas about
      | the origin of the Piri Reis map. A 120k year old ice sheet
      | could mean that humans once lived on Antarctica.
      | 
      | It does make one wonder if any ancient sea fearing humans
      | happened to carve a world map into a durable material such
      | as granite which could have survived until the modern
      | historic era. Maybe such a map, or other mythological
      | artifact fueld the Roman idea of Terra Australis Incognita
      | 
      | /End rampant unsupported armchair speculation
      | 
      | https://en.wikipedia.org/wiki/Piri_Reis_map
      | 
      | https://en.wikipedia.org/wiki/Terra_Australis
 
        | detourdog wrote:
        | The Polynesians used stick maps to identify currents and
        | land masses relative positions.
        | 
        | With no evidence I believe navigation cues were built
        | into the vessel. By keeping celestial bodies aligned with
        | marks on the vessel one can achieve a seasonal calendar
        | as well as documentation on how to modify the
        | configuration for the next leg of the journey.
 
        | contingencies wrote:
        | IIRC the 'maps' made of organic materials were very much
        | a rarity slash teaching aid for the later incarnations of
        | traditional navigation cultures of the Pacific which we
        | have surviving material on. Mostly they used mental maps,
        | and of course the most sensitive instruments available at
        | the time ... at least one example of which was hanging
        | their balls off the edge of the canoe to see if they
        | could detect a temperature shift. A good book on the
        | subject is _We: The Navigators_ though it draws only from
        | one area.
        | 
        | Source: Have a Pacific art collection, have been to most
        | of the major museums on the subject, interested in
        | sailing, authored some of the Wikipedia (featured)
        | articles on related watercraft.
 
        | detourdog wrote:
        | Yes, I would believe that some as fragile as the stick
        | maps was no way to cross an ocean.
        | 
        | What I think is interesting is the physical
        | representation of an oral tradition. This is different
        | than writing as employed today.
 
        | contingencies wrote:
        | Yep. All art is interesting for its relative flattening
        | of multi-dimensional realities in to lesser-dimensional
        | representations. Key concerns for the navigators were
        | signals such as migration patterns, seaweed and other
        | flotsam drift currents, temperatures of said currents,
        | star positions, wave qualities, dominant wind directions,
        | conditions and precipitation and cloud over seasons.
        | These dynamic realities cannot be flattened in to any
        | standard two dimensional representations even today, yet
        | often emanate from or are disturbed by the often-tiny
        | landmasses they would specify as origin, destination or
        | reference points within the navigation problem. In the
        | same way modern navigation uses multi-layered systems
        | like bathymetric maps, local depth sensors, RADAR, GPS
        | and navigation lights to provide orientation and safe
        | passage amongst static and dynamic obstacles, so too the
        | traditional navigators combined layers of sensory input
        | considered too subtle for modern systems yet potentially
        | equally effective in their place and season.
 
        | detourdog wrote:
        | Probably the migratory patterns were as import at as any
        | other reason to travel.
        | 
        | What I seem to be noticing is that the ancients used
        | calculus all the time but it was the geometric tools that
        | they used.
        | 
        | This gave technology a form.
        | 
        | Arabic numerals made tabular data more useful leading to
        | the more number based tools.
        | 
        | This seems to have removed the form from technology.
 
      | renegade-otter wrote:
      | Maybe humans become more developed because it got colder?
      | Even on a country and global scale, the south is usually
      | "behind" the north. It's hot, no one wants to do anything.
      | 
      | The American south (Arizona, Florida) were tiny and
      | unimportant until air conditioning entered the chat.
      | Phoenix was at 100 thousand people in the fifties.
      | 
      | The cold makes us think, the cold make us survive, keeps us
      | on the edge - where we need to be. Respek the cold!
 
        | lukev wrote:
        | This is pretty ahistorical. Most of the world's great
        | civilizations have been from warmer climates. Northern
        | Europe is an exception, not the norm.
 
        | pclmulqdq wrote:
        | All of the world's "great" civilizations come from places
        | with strong seasonality. The ones that didn't have
        | winters had flooding seasons and dry seasons. Some of
        | them had both. It also doesn't need to be bitterly cold
        | for winter to have an effect on crops.
        | 
        | Sumeria and Egypt both had seasonal flooding. Italy and
        | Greece have winters that are cold enough to disrupt
        | agriculture. The Aztecs and Mayans had seasonal floods.
        | The ancient Chinese empires had both. Japan has winters.
        | The list goes on.
 
        | pavlov wrote:
        | On the other hand there's something to be said for a
        | comfortable climate that leaves people with time to think
        | when the everyday isn't a constant complex struggle.
        | 
        | The Inuits of Greenland and Sami people of Lapland didn't
        | have Aristotle or Confucius.
 
        | detourdog wrote:
        | That is only due to writing. I always felt that the high
        | latitude civilizations led to technological development
        | due to the high risk and high solitude.
 
    | downWidOutaFite wrote:
    | It's not scientifically interesting, the glacial-interglacial
    | cycles are pretty well established. I'm guessing they're
    | trying to insinuate some climate change minimalism argument.
 
      | mensetmanusman wrote:
      | It's interesting to know how far back in time the ice will
      | allow them to analyze once they get to the base.
 
    | [deleted]
 
    | rolph wrote:
    | the drilling allows sampling of environmental components over
    | extended period of time. this meas a historic record of,
    | gases, ash, soot, pollen, spores, silt, insects, plant
    | animals, metals, salts.....
 
  | robertlagrant wrote:
  | [flagged]
 
    | WhitneyLand wrote:
    | I'm not aware of any data that supports humans 120k years ago
    | having a significant impact on the earths climate.
    | 
    | I think even our ability to start fire at will is
    | conclusively known to be only ~50,000 years ago.
 
      | detourdog wrote:
      | I always wonder about that natural fission reactor in
      | Gabon. They discovered the Uranium was pre depleted in
      | particular mines.
      | 
      | https://en.wikipedia.org/wiki/Oklo_Mine
      | 
      | Fun to imagine the possibilities.
 
        | angiosperm wrote:
        | That was more than a billion years ago, so no.
 
        | detourdog wrote:
        | I'll take a risk and be skeptical of that claim and see
        | how my life turns out.
 
      | hutzlibu wrote:
      | "Claims for the earliest definitive evidence of control of
      | fire by a member of Homo range from 1.7 to 2.0 million
      | years ago "
      | 
      | https://en.m.wikipedia.org/wiki/Control_of_fire_by_early_hu
      | m...
      | 
      | You don't need to be able to start a fire, when you keep
      | the fire burning all the time. And you can do that, once
      | you control the fire and figure out the difference between
      | dry and wet wood.
      | 
      | Also humans are the dominating species on land since quite
      | a while. Hunting certain species to extinctiom has certain
      | effects on the local ecosystem and globally on the global
      | climate. It all adds up.
      | 
      | But things surely changed in dimension since
      | industrialisation.
 
        | dekhn wrote:
        | People had fire in those times but it's extremely
        | unlikely they produced enough CO2 to have an
        | anthropogenic impact on the climate leading to large-
        | scale temperature changes.
        | 
        | I'm not sure what your perspective on this situation is
        | but I think the case for modern anthropogenic climate
        | change with deleterious effects is based on a wide range
        | of different evidence, and a careful accumulation of
        | facts and analysis. Simply pointing out that humans had
        | fire 2Mya doesn't change the general conclusion about
        | today.
 
        | londons_explore wrote:
        | I suspect gr main change caused by humans >100 k years
        | ago will be wiping out various species and starting fires
        | in seasons and places where fires wouldn't normally start
        | (eg. In places without dry lightning or volcanoes - the
        | only two other ways fires naturally start)
 
    | gameman144 wrote:
    | Just in case this is just a case of word confusion (which
    | I've had before), "anthropogenic" means "caused by humans",
    | not "occurring at the same time as humans".
 
| albert_e wrote:
| what is the risk of uncovering ancient viruses and bacteria from
| permafrost that we don't have immunity to
 
  | hannasanarion wrote:
  | Very very very low. Bacteria and viruses are normally very
  | sensitive to their hosts, they have a kind of symbiosis that
  | means they can't just arbitrarily infect any species they bump
  | into.
  | 
  | Jumping between species does happen, and when it happens it can
  | be a big problem (see COVID-19, Swine Flu), but there is
  | something like _100 million_ different virus species out there
  | [1], and _only 200_ or so are able to infect humans [2].
  | Despite constant interaction between people and all other
  | species of viral host all over the globe, and millions of brand
  | new new virus exposures daily, jumps are still so rare that
  | they are decade-defining when they happen.
  | 
  | 1. https://virology.ws/2013/09/06/how-many-viruses-on-earth/
  | 
  | 2. https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3427559/
 
  | Clamchop wrote:
  | I read a book, How to Clone a Mammoth, by ancient DNA
  | researcher Beth Shapiro.
  | 
  | If what she wrote holds true deep in these glaciers (which take
  | a long time to form so they presumably weren't always buried so
  | deep), then the answer to what the risk may be is "very
  | remote". DNA and RNA disintegrates into very small tatters
  | pretty easily, turns out, frustrating the reconstruction of
  | ancient genomes. Bacteria are definitely dead on multiple
  | counts and viruses will be shredded.
 
  | Archelaos wrote:
  | Here is an article from 2021 that covers that topic:
  | 
  | https://link.springer.com/article/10.1007/s42398-021-00184-8
  | 
  | From the conclusions: "... as shown by recent outbreaks of
  | diseases caused by supposed to be extinct microbial pathogens
  | immured in glacial ice for centuries, there is a serious risk
  | for future epidemics (or even pandemics) to happen more often."
 
  | anon25783 wrote:
  | Negligible. You're far more likely to fall ill from bacteria in
  | your garbage disposal or fungi in your bathroom.
 
| mr-wendel wrote:
| If drilling big holes for scientific research is your thing, I
| suggest https://usoceandiscovery.org/wp-
| content/uploads/2016/06/Casc... as an interesting read about
| earthquakes and tsunamis.
| 
| A quick summary:                 > Geophysical and hydrological
| observatories in sealed boreholes provide a powerful tool to
| understand the hydrology of crustal formations, a means measure
| the hydrologic signal from changes in volumetric strain, and a
| stable site for high quality seismic and geodetic
| instrumentation.
| 
| This data is not just useful on its own, but also when correlated
| to other research. For example, 400+ years ago there was a large
| earthquake
| (https://en.wikipedia.org/wiki/1700_Cascadia_earthquake) off the
| US Pacific Northwest coast (and corresponding tsunami in Japan)
| that is referenced.
 
| almostnormal wrote:
| Two numbers from the article: The oldest ice is 120000 years old.
| The ice is moving at 58 m/years.
| 
| If these numbers are correct the oldest ice has travelled almost
| 7000 km. Greenland isn't that large, and it did not shrink. The
| age estimate is probably correct.
| 
| The speed must have been a lot lower in the past?
 
| ballenf wrote:
| [flagged]
 
| toshk wrote:
| I love humans.
| 
| They somehow decided to start drilling, and not give up & get
| funding for 7 years.
| 
| We are a crazy but exciting bunch of organisms.
 
  | hk__2 wrote:
  | That's because we are social animals. We tend to do things not
  | only for ourselves, but also to contribute to the society we
  | live in.
 
  | uncletammy wrote:
  | > We are a crazy but exciting bunch of organisms.
  | 
  | I read this as "crazy but extinct bunch of organisms"
 
    | mensetmanusman wrote:
    | Also read extinct. Ha. Would be cool to know how to detect
    | and exploit these speed reading induced recognition errors to
    | write things that force people to slow down or go extinct :)
 
| holoduke wrote:
| Would it theoreticaly possible to find frozen animals 120.000
| years old with still intact DNA?
 
  | dekhn wrote:
  | The oldest frozen mastodon found is only 30K years ago.
  | 
  | This isn't really "frozen animals" and everything was sort of
  | mixed together so they had to compare remaining fragments to
  | existing sequences:
  | 
  | https://www.nytimes.com/2022/12/07/science/oldest-dna-greenl...
 
  | sedatk wrote:
  | Yeah, DNA in ice has a half-life of a million years. Seems very
  | much possible.
 
    | wwwtyro wrote:
    | What does half-life mean in the context of DNA? One base pair
    | corrupted / unrecoverable? Half of them?
 
      | netcraft wrote:
      | half life generally means that within the time frame 50% of
      | the material will have been destroyed or changed.
      | 
      | so it would mean that half of the dna might still be
      | available after 1M years
 
        | graycat wrote:
        | To be meaningful, _half-life_ needs a Markov assumption,
        | i.e., that the past and future are conditionally
        | independent given the present. Or, more simply, at each
        | _instant_ , forget the past and for predicting the future
        | use only the present.
        | 
        | Some interesting work in the many contexts where half-
        | life works would be to say what the Markov property says
        | about the mechanism of the _decay_ or whatever are trying
        | to predict in the context.
 
      | monocasa wrote:
      | Half of them. Which is still useful in biological samples
      | that have billions of copies.
 
      | amelius wrote:
      | Yeah, you can still assemble a genome even if strands are
      | broken. In fact this is done all the time as the size of
      | the strands going into DNA sequencers are often only 100s
      | or maybe 1000s of basepairs.
 
    | delecti wrote:
    | Where are you getting that figure? Everything I had ever read
    | on the subject puts the half-life at more like 500 (five-
    | hundred) years. While doing a quick double-check for this
    | comment, it seems there was one sample with the unexpectedly
    | long observed half-life of 15,000 years, still a couple
    | orders of magnitude less than a million years.
    | https://en.wikipedia.org/wiki/Ancient_DNA#Non-human_aDNA
 
      | Tagbert wrote:
      | Preservation conditions might have some bearing.
      | 
      | This recent news article suggests nematodes actually
      | surviving after 46K years in permafrost.
      | https://www.scientificamerican.com/article/46-000-year-
      | old-w...
 
      | sedatk wrote:
      | That's room temperature. Frozen DNA is significantly more
      | resilient. https://www.pnas.org/doi/10.1073/pnas.0702196104
 
      | dekhn wrote:
      | I'm not an expert in this area but I do know a fair amount
      | on the subject. I believe the section you linked is out of
      | date.
      | 
      | The DNA we get back from old situations typically was
      | preserved, by dryness/freezing, and it's still quite
      | fragmentary. The actual "half life" of DNA is not that
      | interesting- its the details of the DNA remnants that
      | matter.
 
  | tokai wrote:
  | Not an animal, icecore, or that old, but ancient plants has
  | been grown from seeds from permafrost.[0] So who knows what
  | might be found and analyzed from all the icecores.
  | 
  | [0] https://www.theguardian.com/world/2012/feb/21/russian-
  | scient...
 
  | AmericanOP wrote:
  | [flagged]
 
    | bagels wrote:
    | I don't think this is a factual response. This appears to be
    | some cartoon?
 
      | AmericanOP wrote:
      | Recent Netflix story arc about boxing a defrosted
      | caveperson. I couldn't resist.
 
        | mandmandam wrote:
        | Not even a caveperson - a 200 million year old dude who
        | fights tyrannosaurs.
        | 
        | It's ridiculous and it's awesome.
 
| [deleted]
 
| roter wrote:
| At approximately the same depth drilled, Antarctica e.g. EPICA @
| Dome C yields _8_ interglacials [0].
| 
| [0]
| https://en.wikipedia.org/wiki/European_Project_for_Ice_Corin...
 
| ChuckMcM wrote:
| This is a very important project. There is a joke in here about
| "why not wait 2 years for the ice to melt off if you wanted to
| look at the mud underneath?" But as the article states, _" 'This
| will change climate models because it redefines our basic
| understanding of how ice moves,' explains Dorthe Dahl-Jensen."_
| Much, if not the majority, of climate science is the creation of
| models (differential equations mostly) that describe the
| "response to influence" of the big chunks of things that cause
| the climate on the planet. The better the model, the better able
| we are to guess what will happen next (which is sorely needed in
| a system where you cannot control the input variables by
| declaration).
| 
| One of the big unknowns in the model is "where will the clouds
| show up?" That unknown stems from our understanding of the water
| capacity of air by temperature, the increase in air temperature
| leads to the air holding more water, and water is the basis for
| cloud formation. If the clouds form "low" they increase albedo
| and create colder temperatures, if they form "high" they act as a
| semi-mirrored surface and reflect light that has been reflected
| from the surface back down for another shot at generating heat.
| 
| Much of the IPCC's work has been done in MATLAB[1,2] so if you
| have a reasonably powerful workstation you can play around with
| various initial conditions and settings yourself to see what
| might happen in the future.
| 
| No matter what the far future holds, the near future holds more
| violent storms as storms are powered by the temperature
| differentials of the air, land, and sea.
| 
| It is of note (for me, probably not for many others) that we
| don't have good models for how an ice age starts. There are a few
| papers that talk about ice ages being a response to warming (hit
| a tipping point, generate clouds, and get a "nuclear winter"
| scenario without the nuclear part). But much of the nuclear
| winter work has been refined and that scenario is generally
| considered unlikely AFAICT from what people seem to be publishing
| these days. Turco's work[3] and things that cite it are a good
| jumping off point if you want to read up on that. It isn't
| perfect because smoke/soot are not clouds (different albedo
| numbers, different cooling attributes) but the accumulation and
| dispersion of atmospheric obstructions is solid stuff.
| 
| [1] Some code and information used to generate plots in the IPCC
| reports -- https://github.com/IPCC-WG1/Chapter-9
| 
| [2] Mathworks trying to get you to buy their climate data toolbox
| -- https://www.mathworks.com/discovery/climate-stress-
| testing.h...
| 
| [3] Climate and Smoke: an Appraisal of Nuclear Winter --
| https://www.science.org/doi/abs/10.1126/science.11538069
 
  | samstave wrote:
  | It would seem to me, that the best way to do long-scale climate
  | models of a body ; knowing its composition in layers over time
  | is really important to be able to calculate the flow of the
  | layers of composition as particles.
  | 
  | Think of the experiment of light as wave/particle...
  | 
  | Glacial/geological scales operate as thus ; as physical masses
  | of particles, but move in more wave-like manners - so you'll
  | have material suspended and located in the overall mass based
  | on how they were consumed as a particle, but the characterists
  | of the glacial mass will appear to be acting like fluid waves.
  | 
  | So maybe if you know the timeline of a glacial flow, you can
  | predict where the most particulate-glacial-slurry is held (thus
  | minerals, biologic wash off in certain events etc.
 
  | anigbrowl wrote:
  | A lot of modeling is moving toward Julia, so if you don't want
  | to give money to Mathworks here are some alternatives:
  | https://juliaclimate.github.io/Notebooks/
 
    | javajosh wrote:
    | Note that the individual license for Matlab is $149/year [0],
    | which isn't crazy IMHO.
    | 
    | 0 - https://www.mathworks.com/pricing-
    | licensing.html?prodcode=ML...
 
      | __MatrixMan__ wrote:
      | Given the added burdens of...
      | 
      | - managing licenses across multiple devices
      | 
      | - limiting the people you can share code with to ones that
      | are willing to deal with licenses
      | 
      | - budgeting for an ongoing subscription / renewing as
      | needed
      | 
      | ...I'd say that even $10/year is too much. Ecosystems that
      | create collaboration barriers like these are no place for
      | important work.
 
      | anigbrowl wrote:
      | Agreed, it's sofa change for an institution. But I remember
      | cost being a big obstacle when I first wanted to learn
      | serious programming around 1990, so I feel like free
      | programming languages are better.
 
        | analog31 wrote:
        | The institutional cost is more AFAIK, but should still be
        | pocket change -- one productive week pays for it. But the
        | price is just high enough to trigger all sorts of weird
        | management wastes. Especially if you envision wanting
        | more than one installation, or are in an austerity-
        | culture organization.
        | 
        | While you're dealing with the time and aggravation of
        | budget approval and recurring license management, I've
        | got my Python and Arduino toolchains installed on
        | literally every computer that I touch: At home, my
        | office, the labs, etc.
 
      | cstejerean wrote:
      | Without any toolboxes though, and you'd typically need a
      | handful of those depending on what field you're working in
      | and that's another $45 per toolbox. But also anyone just
      | getting started may not know which toolboxes they need
      | upfront which increases the uncertainty about the price.
      | 
      | I really wish they had a more reasonably priced all you can
      | eat home license that included all toolboxes.
 
    | ChuckMcM wrote:
    | I have moved all my "matlab like" work (mostly signal
    | processing) into Octave for that same reason.
 
      | tetris11 wrote:
      | GNU Octave is surprisingly good. I had old MATLAB work from
      | university that I wanted to revisit for teaching purposes,
      | and was surprised by the lockout imposed by the pricing
      | model of MathWorks[1] (120 EUR for an individual license,
      | 260 EUR for teaching)
      | 
      | 1: https://nl.mathworks.com/pricing-
      | licensing.html?prodcode=ML&...
 
  | earthscienceman wrote:
  | You're adding important context but I would like to clarify
  | something to highlight just how complex climate change really
  | is. I also am going to make a few related comments, as I do
  | most of my research on melt in Greenland. Full disclosure: I do
  | know some of the people in this article but I have never been
  | to eGRIP specifically. I will be in Greenland in a week nearby
  | though.                  No matter what the far future holds,
  | the near future holds more violent storms as storms are powered
  | by the temperature differentials of the air, land, and sea.
  | 
  | This is true, sort of. There's a lot nuance needed for this
  | broad statement. In particular, "Arctic amplification" means
  | that the pole-to-equator temperature gradient is actually
  | weakening. If you were inclined to believe the covid lab leak
  | theory you would also be inclined to jump on this and say "then
  | the extreme storms are nonsense". However, what's really
  | happening is that the waves in the upper atmosphere ("Rossby
  | waves") are getting more wave-y. Which is really saying that
  | additional energy from CO2 warming is resulting in stronger
  | transport and more significant variability. It's _not_
  | resulting in larger gradients. Although sometimes the gradients
  | are also extreme.
  | 
  | Climate is a question of two things, time scales and spatial
  | scales. Dumping a bunch of CO2 in the atmosphere messes with
  | both.
  | 
  | I also want to point out that this isn't the first time a core
  | has been dug to the bed of the Greenland ice sheet. It's also
  | not the second. Some comments seem to be implying this. I have
  | a bad taste for science reporting/announcements like this that
  | fail to provide context. Of course this is important work but
  | it's following up and improving on several previous deep core
  | drilling experiments. We still have many samples from these
  | previous cores. This is still a very good thing to research and
  | will hopefully provide important new insight. But there is
  | significant previous work it builds on [1]. And the title kind
  | is vague enough that outsiders/the public might not understand
  | that.
  | 
  | Also also, to be a little vitriolic, the IPCC Matlab code is a
  | crime against humanity and fuck Mathworks.
  | 
  | [1]https://www.sciencedaily.com/releases/2021/03/210315165639.h
  | ...
 
    | photochemsyn wrote:
    | I'd add that although the intergrated yearly _average_ pole-
    | to-equator gradient is indeed weakening, in terms of extreme
    | storms this probably doesn 't matter since the gradient is
    | still very strong in winter months in the Northern
    | Hemisphere, and if you pump the atmosphere with more water
    | vapor from the tropics, then intense seasonal storms and
    | extreme flooding can be expected for at least half the year
    | in the Northern Hemisphere - and in midlatitudes, the east-
    | west motion of frontal systems complicates the issue further
    | (though it seems increased water vapor is driving that engine
    | more than anything else).
    | 
    | The Artic amplification effect appears to be having a big
    | effect in the summer months as the decreased gradient allows
    | the polar jet stream to meander southwards, resulting in
    | random persistent blocking events (responsible for recent
    | spate of heat waves) related to Arctic amplification effects
    | on the jet stream (in both hemispheres). Good discussion
    | here:
    | 
    | https://www.carbonbrief.org/jet-stream-is-climate-change-
    | cau...
 
    | sleet_spotter wrote:
    | Also work on ice, though not with cores. Just 2nd'ing this as
    | being a great point. Arctic amplification is fascinating and
    | IMO understudied relative to its importance.
    | 
    | The distinction I believe the article is trying to make
    | around the "first-core-to-ground" sentiment, is that this is
    | the first time a core has been drilled through the full
    | thickness of an ice *stream*. These are regions of an ice
    | sheet with very rapidly moving ice. Ice loss from ice streams
    | may have a larger and more immediate impact on sea level than
    | other regions in Greenland and Antarctica. However, I do not
    | actually know whether this is the first core drill ed through
    | an ice stream, but I'm assuming that was the article's
    | intent.
 
  | wing-_-nuts wrote:
  | Wow, thanks for the links, this is _really_ neat
 
  | aeroman wrote:
  | As a "cloud person", I just want to add a few things to the
  | description of how clouds affect the climate (and why high
  | clouds have a wamring effect).
  | 
  | All clouds are white, so they all reflect sunlight back into
  | space (during the day), cooling the Earth.
  | 
  | All clouds are (almost) black in the infra-red, meaning the
  | amount of energy they emit in the infra-red is determined by
  | their temperature. Colder clouds emit less energy.
  | 
  | Almost all clouds are colder than the surface beneath them,
  | which means they emit less infra-red energy to space than a
  | clear day would. This reduces the amount of energy the Earth
  | emits to space, so warming the climate.
  | 
  | High clouds are colder than low clouds, so have a stronger
  | warming effect.
  | 
  | In summary:
  | 
  | Low clouds - Reflect sunlight (cooling), don't trap much infra-
  | red (little warming)- Net: Cooling effect
  | 
  | High clouds - Reflect sunlight (cooling), trap lots of infra-
  | red (stronger warming) - Net: Warming effect
 
    | photochemsyn wrote:
    | This IR satellite view of clouds and water vapor centered
    | over N/S America is pretty nice. You can also see the daily
    | pulse of cloud formation over the Amazon rainforest:
    | 
    | https://youtu.be/f7QttjGu628?t=142
 
    | kfrzcode wrote:
    | I will give you the benefit of doubt given it's Hacker News
    | you likely are an expert, but this feels like one of those
    | "sounds too intuitive to be that simple" type complex
    | factors. Any literature on the topic from which I can improve
    | my understand?
 
    | Ilnsk wrote:
    | I wish I were a cloud person.
 
      | Insanity wrote:
      | When I read that first sentence, I thought "what has cloud
      | (software) to do with this"
 
        | Nevermark wrote:
        | Not series, maybe a bit serious:
        | 
        | Cloud computing energy use appears to be on an
        | exponential trend driven by general trends (all things
        | automated), with new forms of automation compounding
        | competitive pressures (deep learning models quickly
        | getting larger, more powerful, more useful, and more
        | versatile in a way erasing many lines holding back past
        | competition.)
        | 
        | At some point, it seems inevitable that computing usage
        | will be a first level climate driver, regardless of how
        | green the energy is.
        | 
        | Harnessing orbital solar, fission and fusion power, may
        | solve the CO2 energy problem, without requiring us to
        | steal the biosphere's energy needs, but will eventually
        | create a massive waste heat energy problem.
        | 
        | Unless we find someway to efficiently transfer mass
        | amounts of heat energy off of Earth.
        | 
        | Or we eventually limit computing on Earth, and export
        | that to the Moon and beyond.
 
    | almostnormal wrote:
    | * * *
 
    | crznp wrote:
    | That's interesting. How relevant is energy transport in
    | comparison to the optical effects?
    | 
    | Eg: my understanding is that hurricanes are net cooling
    | because they transport heat from the ocean surface to the
    | upper atmosphere. Presumably the same can be said for
    | cumulonimbus/thunderheads? Or perhaps it is more relevant
    | when they form in the day and when they dissipate at night?
 
| m3kw9 wrote:
| Have a drink?
 
| [deleted]
 
| bobske3 wrote:
| At the mountains of madness
 
| CrzyLngPwd wrote:
| [flagged]
 
| samstave wrote:
| There is a design for an ice-melting-slurry-bot that could be
| made, where the outer diameter of the bore is melted by
| heat/lasers - where the lasers/heat is also projected into a cone
| at the point of the bore-ing machine, where the center pipe is a
| vacuum to slurp up the slurry as it melts the ice around the
| bore-head...
 
  | hanniabu wrote:
  | That would ruin the core samples
 
    | samstave wrote:
    | We dont want the core samples intact (we want to kill
    | microbiologics on the way down to the goal, which is the
    | crust and determination for other vacuous caverns under the
    | ice, via both vertical and horiz boring. and cameras in
    | crytal lenses to withstand the heat or polarize against the
    | lightwaves of the lasers such that they are clear and a good
    | image can be seen.
    | 
    | /Sci-fi..
    | 
    | My original comment is my idea based on the 1960s patents for
    | nuclear tunnel boring machines which use the reactor heat to
    | exchange the tunnel walls to molten glass... (And I am really
    | into DUMBS - as are many)
    | 
    | https://patents.google.com/patent/US3885832A/en
    | 
    | There are a lot of patents like this - so dont think this
    | line of thought was abandoned, Hello Musk's Boring company...
    | Good thing hes connecting State on a Deep level.
 
  | BenjiWiebe wrote:
  | You aren't going to be able to vacuum slurry up from several km
  | down.
 
    | bequanna wrote:
    | Even with a very small diameter hose/pipe?
 
      | qbrass wrote:
      | The smaller pipe has less water in it, but the surface area
      | the vacuum can act on is also smaller so the column of
      | water equals out the same as with the larger pipe.
      | 
      | At sea level, that's about 30 feet deep. If you want to
      | bring water up from deeper, you have to move the pump down
      | the well and push the water up the pipe instead of trying
      | to suck water up like the pipe's a straw.
 
| dclowd9901 wrote:
| I've always wondered: what do they do if the shaft snaps
| somewhere in the middle?
 
  | aio2 wrote:
  | This is more for oil drilling, but this is a possibility.
  | https://www.drillingformulas.com/fishing-drill-pipe-procedur...
 
  | sleet_spotter wrote:
  | I'm not totally sure how systems work for drilling this deep,
  | but typically ice core setups attach the coring apparatus to
  | the surface via a cable that is spooled by a winch. The cable
  | itself ends up being the heaviest part of the system.
 
| sdfghswe wrote:
| Can't believe they don't show a photo of what appears to be a 10
| meter in diameter, 2.7km deep hole.
 
  | FredPret wrote:
  | There's a bright future in big holes.
  | 
  | Imagine what we can get our hands on if we could find a nice,
  | cheap way to dig 10+ km down all over the place. The mantle is
  | 2000+km thick. Our deepest mines are 3-4 km deep.
  | 
  | We could also harvest a ton of heat this way - and maybe even
  | use it for garbage disposal. Master Of Orion 2 had the Deep
  | Core Mines and Core Waste Dumps - maybe that's the way to go!
 
    | TechBro8615 wrote:
    | Is the idea of using a big hole for garbage disposal that we
    | would dump the garbage into the molten core and let it burn?
    | Or is it more about using the hole as a really deep landfill?
 
      | hinkley wrote:
      | Do you know what a hole from the surface to the molten core
      | is called?
      | 
      | An active volcano.
 
        | TechBro8615 wrote:
        | Yeah, I realized that after I commented, and when I
        | googled it, the Quora answer I got basically _boiled down
        | to_ "you don't know what will come back out."
 
        | hinkley wrote:
        | I always thought that was the scary part of a nuclear
        | plant meltdown until I watch Chernobyl and realized
        | poisoning the aquifer for a million years is a much more
        | likely scenario.
 
        | FredPret wrote:
        | Scary thought but you'd (have to) stop digging way above
        | the molten part.
        | 
        | It heats up way above 100C long before you get there,
        | which should be plenty for geothermal energy.
        | 
        | I wonder if sustained high temperature exposure would
        | gradually decompose plastic / toxic waste / other bad
        | things into less harmful components.
        | 
        | Of course, heavy elements came from down there, so it's
        | probably not an issue to dump them back down. Just stay
        | well clear of the water table!
        | 
        | I am of course not a geologist, and it'd be interesting
        | if one could give a perspective on this.
 
        | hinkley wrote:
        | I'm not sure how tall a column of water you need to
        | trigger supercritical water oxidation, but the problem
        | would be getting the oxygen down there.
        | 
        | Better to do that stuff at the surface, I think.
 
  | tokai wrote:
  | Its more like 5cm in diameter.
 
  | TheRealPomax wrote:
  | Ice cores are a few inches across. The photo at the top of the
  | article is not of the drill hole but of the hole they had to
  | dig in the snow to get to the ice they actually drilled.
  | 
  | See the photo of the final ice core [1] to see how miniscule
  | the actual drill hole is.
  | 
  | [1] https://science.ku.dk/english/press/news/2023/pay-dirt-
  | for-i...
 
    | blackkettle wrote:
    | The article definitely makes it sound like they had "boots on
    | the ground". There's a picture of muddy boots and the caption
    | says they are covered in ancient mud.
 
      | TheRealPomax wrote:
      | You need to clear a lot of snow before you can stand on the
      | ice that you're drilling in (You can't drill straight if
      | your rig's sitting on snow, you need to dig until you hit
      | solid ground, and in this case the ground is ice). That's
      | the "boots on the ground" part. They were physically there
      | to do the drilling (as opposed to giant automated core
      | drillers such as DISC[1], which don't require "boots on the
      | ground" so much as they just require one or more operators
      | to oversee operation)
      | 
      | The ancient mud's from hauling up the ice cores, not from
      | standing 3 kilometers deep in a giant hole.
      | 
      | [1] https://icedrill.org/equipment/deep-ice-sheet-coring-
      | drill
 
      | tokai wrote:
      | That mud came up with the last core.
 
    | Giorgi wrote:
    | Why is is black and white though? also - how do they transfer
    | energy to drill down 2.7km? or how the hell does it work?
 
      | TheRealPomax wrote:
      | See other comment, and "that's a fun thing to check youtube
      | for", respectively =)
 
      | tgamma wrote:
      | As mentioned in the article, the core was handled under red
      | light to prevent any potential damage. Perhaps the decision
      | to convert the photograph to black and white was made
      | because otherwise it would have been black and red.
 
  | dewey wrote:
  | It's a bit hidden but there's at least a few cool pictures in
  | the "Facts about the EGRIP camp" section (Click the + icon).
  | 
  | There you can see that the actual hole is ~10cm in diameter and
  | the actual drilling site under the snow.
 
  | jtsiskin wrote:
  | Or a video dropping a rock into it
 
  | hinkley wrote:
  | The camera wouldn't take the picture, and then several of the
  | scientists had to be sedated as they started acting strangely.
 
    | j1elo wrote:
    | As long as they don't come up with schematics to build a
    | white Marker...
 
      | hinkley wrote:
      | For all we know that could be psyops by Lovecraft. Maybe
      | it's not a white marker, it's a blue beacon.
 
  | giantrobot wrote:
  | What an ice hole.
 
  | JimtheCoder wrote:
  | To be fair, is a photo of a hole that interesting?
 
    | peoplearepeople wrote:
    | yes, people love pictures
 
    | mbfg wrote:
    | Here's a picture of a cat sitting on the hole.
 
    | iknowSFR wrote:
    | [flagged]
 
      | CrzyLngPwd wrote:
      | Yes, but they may share wetness this one does not share the
      | warmth.
 
        | jprd wrote:
        | https://old.reddit.com/r/trypophobia/
 
        | cancerboii wrote:
        | [dead]
 
| robotnikman wrote:
| >electromechanical drill designed to take 122 mm (4.8-inch)
| diameter ice cores
| 
| Interesting that they choose 122mm as the core size when
| designing the drill. It makes me wonder if its built from a
| decommissioned and repurposed 122mm artillery gun barrel.
 
| johnnyApplePRNG wrote:
| That's a rate of about 4.3 centimeters per hour.
| 
| Can anybody elaborate as to why this process takes so long?
 
  | klyrs wrote:
  | I've never drilled a hole with 10m diameter before, but I
  | imagine they've been more careful about taking and studying
  | cores than you were.
 
    | Zamiel_Snawley wrote:
    | Surely you mean 10cm?
 
      | klyrs wrote:
      | My word. I and at least one other poster here were misled
      | by the picture at the top of the article.
      | 
      | But, for whatever it's worth, a trip to Wikipedia tells me
      | that they took 2 years off, due to covid.
 
        | joshvm wrote:
        | It's more realistic to say that covid caused logistics
        | issue two summers in a row. The first summer was
        | presumably 2020 when almost every country locked down. In
        | 2021 things weren't much better and the various polar
        | programs were dealing with both caution and a backlog of
        | issues from the previous year.
        | 
        | The actual downtime may have been significantly less than
        | 24 months but still could have killed progress for 36.
        | There's a pretty small window that you can deploy for
        | these sorts of operations.
 
  | roter wrote:
  | Did you store the tube of ice?
 
  | sleet_spotter wrote:
  | As the hole gets deeper, the amount of time to bring up core
  | sections and send the drill back down become significant. That
  | combined with the previously mentioned short field season.
  | Drilling more than a few hundred meters becomes very difficult
  | logistically as well, especially in such a remote setting.
 
    | mywittyname wrote:
    | Like fetching the n-th element from a linked list by starting
    | at the first node.
 
    | foota wrote:
    | Who knew, drilling is O(N^2)
 
      | hcnews wrote:
      | It's not O(N^2) is it? It can be a continuous line of ice
      | being pushed up. Depending on the weight bearing ability of
      | the lift and digging capacity, you would figure out a fixed
      | distance after which you would place the buckets to carry
      | up the ice.
      | 
      | Its an interesting interview question at the very least.
      | (More complications arise as and how you get deeper into
      | the ice).
 
        | [deleted]
 
  | altacc wrote:
  | It's not a continuous 24/7/365 process. They have a drilling
  | season each year, I believe about 6-8 weeks, have drilled at 2
  | different sites and been interrupted by the pandemic.
 
    | jppope wrote:
    | why was ice drilling interrupted by the pandemic?
 
      | applied_heat wrote:
      | Getting supplies such as food and shift changeovers?
 
      | eastbound wrote:
      | Well it was forbidden to walk outdoors. People were fined
      | by helicopter is all Western countries for walking alone in
      | forests, dunes or farmland.
 
  | lexicality wrote:
  | it's a very high aspect ratio hole (267:1) so they have to
  | peck-drill it and it takes a very long time to lift the
  | drillbit to remove the swarf from the end
 
  | [deleted]
 
  | drKarl wrote:
  | I believe the deeper the layer of ice, the thougher it is, so
  | at the surface is relatively easy to drill but at those depths
  | it might be like drilling on steel.
 
| stainablesteel wrote:
| so how do they know its not just a big rock covered in frozen mud
| with more ice below it
 
| ultrablack wrote:
| [flagged]
 
  | chrisco255 wrote:
  | Given that Greenland regularly gains surface mass, even this
  | year gaining close to 50 gigatons as of June 20th:
  | https://nsidc.org/greenland-
  | today/files/2023/06/SMB_Fig3_15J..., you might have to wait a
  | few more millenia or even another 100K before the next
  | interglacial.
 
    | fg__ wrote:
    | [flagged]
 
| marcosdumay wrote:
| Please, if the title is going to be that, at least remove the
| capitalization from that "m", so it represents an unity instead
| of "millions of something undisclosed".
 
  | dang wrote:
  | Submitted title was "Researchers reached the bottom of ice
  | sheet at -2670m after 7 years of drilling". I've reverted to
  | the article title now, or rather a slightly rewritten version
  | to omit the linkbait.
  | 
  | Our software did screw up the m->M thing. Sorry!
 
  | porphyra wrote:
  | Also, a space is needed.
  | 
  | > The numerical value always precedes the unit and a space is
  | always used to separate the unit from the number.
  | 
  | The International System of Units. 9th edition, section 5.4.3,
  | page 149. https://www.bipm.org/en/publications/si-brochure
 
  | JimtheCoder wrote:
  | "so it represents an unity instead"
  | 
  | If you are going to be pedantic, that "an" should be an "a",
  | no?
 
    | ksd482 wrote:
    | That's what I was thinking, yes.
    | 
    | You have to think HOW you pronounce the word. The 'u' in
    | "unity" is pronounced as "you" which starts with a consonant.
    | Hence, you use 'a' not "an".
 
      | lopis wrote:
      | I've always wondered this, as a non English native speaker.
      | You could also say the "u" in unity is pronounced as "iu"
      | which starts with a vowel and sounds the same as "you", so
      | your reasoning sounds incorrect. Perhaps a better
      | explanation is that the "iu" diphthong is already paired
      | together, so attaching it to the "an" sound to form "aniu"
      | doesn't roll off the tongue as well.
 
        | hunter2_ wrote:
        | Correct, this particular diphthong and the substitution
        | of "an" for "a" serve the same exact function, so having
        | both would be redundant. If we were to look at a word
        | that starts with u but doesn't have the diphthong, such
        | as Ubuntu, then "an" is used.
 
      | hunter2_ wrote:
      | I think unity is just a typo for unit, not that that
      | changes this discussion.
 
      | tokai wrote:
      | But Y is a vowel?
 
        | chungy wrote:
        | English rules for using "a" or "an" depend on sounds used
        | in the next word, not particular letters. "A unit" and
        | "An hour" are easy examples that might trip people up
        | when focused on the letters used in spelling, but if you
        | sound it out, you can probably work out what sounds best.
 
        | ad133 wrote:
        | And of course it's even more complex when you mix UK vs
        | US English:
        | 
        | - an herb (US), where the "h" is silent
        | 
        | - a herb (UK)
        | 
        | Cue confusion about "an historic".
 
        | lcnPylGDnU4H9OF wrote:
        | Yeah, occasionally. The previous sentence uses it as
        | both.
 
        | JimtheCoder wrote:
        | Sometimes...
 
        | stronglikedan wrote:
        | Only when your mouth parts move a certain way to pronouce
        | it: https://www.youtube.com/watch?v=I6As7KhrFQ4
 
  | giuliomagnifico wrote:
  | Hacker News capitalized the "M" by itself.
 
  | 6D794163636F756 wrote:
  | Thank you for pointing this out. I thought it was referring to
  | the age of the samples taken before reading your comment. It
  | made the abstract less disappointing.
 
    | marcosdumay wrote:
    | I only clicked on the article because I thought it was the
    | age of the samples too.
 
      | adolph wrote:
      | If something has a negative age, does that mean it is from
      | the future?
 
        | stefncb wrote:
        | I can't tell if you're joking, but negative numbers are
        | used to represent years BC.
 
        | adolph wrote:
        | It responds to the comment "I only clicked on the article
        | because I thought it was the age of the samples too." Age
        | is "The length of time that a person or thing has
        | existed." AD and BC are both absolute values from a zero
        | point, both positive ("1 BC is year 0, 45 BC is year -44"
        | [0]). A relative chronological dating by some
        | phenomenological method such as radiocarbon or
        | thermolumenescence might establish a negative date
        | relative to some other known benchmark [1].
        | 
        | How might something dated from the future be found? I'm
        | not certain, but maybe it has to do with aliens that are
        | all the rage nowadays.
        | 
        | If I were 12 years old, I would have been born 12 years
        | ago.                  2023       -  12        ----
        | 2011
        | 
        | If I were -12 years old, I would be born 12 years from
        | now.                  2023       - -12        ----
        | 2035
        | 
        | 0. https://en.wikipedia.org/wiki/Anno_Domini
        | 
        | 1. https://en.wikipedia.org/wiki/Chronological_dating
 
| Scofield67 wrote:
| [flagged]
 
___________________________________________________________________
(page generated 2023-07-31 23:00 UTC)