Climate Science Glossary

Term Lookup

Enter a term in the search box to find its definition.

Settings

Use the controls in the far right panel to increase or decrease the number of terms automatically displayed (or to completely turn that feature off).

Term Lookup

Settings


All IPCC definitions taken from Climate Change 2007: The Physical Science Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Annex I, Glossary, pp. 941-954. Cambridge University Press.

Home Arguments Software Resources Comments The Consensus Project Translations About Donate

Twitter Facebook YouTube Pinterest

RSS Posts RSS Comments Email Subscribe


Climate's changed before
It's the sun
It's not bad
There is no consensus
It's cooling
Models are unreliable
Temp record is unreliable
Animals and plants can adapt
It hasn't warmed since 1998
Antarctica is gaining ice
View All Arguments...



Username
Password
Keep me logged in
New? Register here
Forgot your password?

Latest Posts

Archives

The Last Interglacial Part Three - Melting Ice and Rising Seas

Posted on 10 August 2011 by Steve Brown, jg

NOTE: This is the third article of a five-part series on what we can learn from the Last Interglacial time period. Understanding this period may provide clues on how the environment may respond to similar conditions in the future. In the first post, we described the conditions that exisited during the Last Interglacial. In the second post, we looked at the key factors for making it a warm period. In this post, we examine two of the most profound environmental impacts that resulted from the warm climate.

In the previous posts we learned that the Last Interglacial, also known as the Eemian in Europe, was significantly warmer than today in large regions of the Northern Hemisphere, and may have been around 1oC warmer globally.  The main reason for this warmer climate was an increased amount of energy from the Sun being received at high northern latitudes due to Earth's orbital configuration, plus Earth had an increased capacity to absorb heat due to vegetation changes and reduced ice and snow cover.  The period is also known for global sea level being several metres higher than today.  So how high did sea levels get and why?

Contrary to what common sense might tell you, global sea-level is not the same everywhere and can vary by many metres from region to region.  Seawater can bulge up in regions under local gravitational influence due to proximity of land masses, undersea mountains, or even due to changes in atmospheric pressure.  Physical properties of the sea water such as temperature and salinity will affect its density and hence the volume it occupies.  Sea level also depends on the actual amount of water in the oceans, which can be altered significantly during the course of glacial/interglacial cycles depending on the mass of water locked up in glaciers and ice-sheets.

The IPCC AR4 report describes evidence from a variety of sources that suggests either a partial or a complete disappearance of the Greenland Ice Sheet during the Last Interglacial, providing a contribution of 2 to 4 m of sea-level rise.  This was likely over a period of several thousand years in conjunction with an Arctic summer warming of up to +5oC.   There is uncertainty in the interpretation of Greenland ice core records, though it does seem likely that the Greenland Ice Sheet lost at least half of its volume and the top of the ice sheet in the Summit region may have been 500 m lower than the present day.   Otto-Bliesner et al. (2006) simulated the behaviour of the Greenland Ice Sheet in response to the known climate forcings of the Last Interglacial.  They found ice melt configurations consistent with palaeo-records of the Greenland environment, which suggest a sea-level rise contribution of 2.2 m to 3.4 m (Figure 1).  The Greenland Ice Sheet melt is very sensitive to warm summers, which is what resulted from the particular orbital forcing configuration of the Last Interglacial.

Last Interglacial Greenland Ice Sheet Simulation

Figure 1: Simulated Greenland Ice Sheet thickness maps.  Configuration A gives a minimum sea-level contribution of 2.2 m.  Configuration B gives a maximum sea-level rise of 3.4 m likely contributed by the Arctic. (Otto-Bliesner et al. 2006)

It's likely that summer sea-ice persisted in the Arctic Sea, though remains of plankton obtained from sediments on the Lomonosov Ridge suggest that there were extensive areas of open sea for periods of the Last Interglacial (CAPE-Last Interglacial Project Members, 2006).  Other proxy records, mainly derived from marine sediment cores, suggest that there were warmer than normal seas in many parts of the oceans that contributed to the melting of Arctic sea-ice.  Though melting sea-ice does not directly affect sea levels, it does result in more of the Sun's energy being absorbed by the oceans as there is no longer any reflective ice.

It's long been understood that global sea level reached over 5 metres above that of the present day, however some research published over the past decade has indicated that sea-level may have peaked at over 9 metres before the end of the Last Interglacial.  Because the Greenland Ice Sheet melt is thought to have contributed to no more than 4 m of sea-level rise, it may imply a contribution from melting of the Antarctic Ice Sheet to account for the additional sea-level rise. 

Coral reefs can provide a highly accurate measure of past sea-levels, as coral grows close to the surface where there is plenty of light and will always grow upwards with rising sea level. When sea-level reaches a maximum, erosional processes at the shoreline will leave tell tale marks that can be used to identify these maximum sea-levels. Coral can also be dated accurately using isotopic analysis, which means that the dates of sea-level maxima and minima can be derived with some precision.  Figure 2 shows a reconstruction of a series of Sea-Level Intervals (SLI's) by Hearty et al. (2007), using geological and coral reef analysis from 15 sites worldwide. The brief regression at 125 ka [fig 2: SLI 3] seems to have reversed within 1000 years implying a decrease in polar ice possibly from the Greenland Ice Sheet. The rapid sea-level rise that then ocurred from 121 to 119 ka suggests to the authors a rapid collapse of the Greenland and West Antarctic Ice Sheets. They suggest that the associated rapid release of meltwater would have significantly altered the thermohaline circulation leading to enhanced temperature gradients between cool temperate latitudes and the hot tropics, which potentially led to intensified weather systems and increased storminess. Evidence in Barbados of intense storms, or possible local tsunami activity, is suggested by trees buried by dunes in living position and the deposition of huge boulders on top of Last Interglacial sediments (Hearty & Neumann, 2001; Hearty et al., 2007) 

 

MIS 5e Sea-Level Fluctuations 


Figure 2: Reconstruction of Last Interglacial sea-level intervals 1 – initial postglacial rise at ~130ka, 2 -  +2.5 m at 132-125 ka, 3 – brief regression at 125 ka, 4 – rise above +3 m between 124-121 ka, 5 – rises to +9 m from 121-119 ka, 6 – rapid retreat of sea-level at end of MIS 5e. (Hearty et al., 2007)

Some caution should be taken with these higher estimates of sea-level rise as assumptions have been made on the past rate of tectonic uplift at many of the sites used for sea-level palaeo-studies.  Possibly the most useful assessment so far is by Kopp et al. (2009), who analysed a catalogue of sea-level indicators for the Last Interglacial and provided a statistical estimate that there is a 95% probability that global sea-level reached at least +6.6 m, and a 67% probability that sea-level was at least +8.0 m, but only a 33% probablity that it exceeded 9.4 m compared to the present. 

Estimated Sea Levels during the Last Interglacial

Figure 3: Estimated sea levels during the Last Interglacial

Colville et al. (2011) analysed the sediment in cores retrieved from the Ocean bed that was transported to the sea from Greenland by glacial processes.  They were able to isotopically identify the specific regions of Greenland that the sediment came from and hence were able to estimate the extent of the Greenland Ice Sheet during the Last Interglacial.  Surprisingly, they find that much less of the Greenland Ice Sheet melted compared to earlier estimates and that the contribution to sea-level rise was no more than 2.2 m.  This leads to the conclusion that the contribution from Antarctic ice-melt was much higher than previously thought.  Another very recent paper by McKay et al. (2011) that was highlighted in a recent SkS post comes to a similar conclusion.  This time, though, from a study that finds that the contribution to sea-level rise from the thermal expansion of seawater was much lower than previous research due to a lower estimate of sea temperature during the Last Interglacial, with an increased contribution from Antarctica to make up the balance.  This raises the spectre of Antarctica being far more sensitive to melting than we thought. 

Earth during the Last Interglacial climatic optimum

Figure 4: An impression of how Earth might have looked during the Last Interglacial

Ocean circulation is pivotal in its role for transfering heat around the globe, as well as being a significant factor in regional climate and weather patterns.  Did the large volume of cold freshwater that returned to the ocean from the melting ice sheets affect this circulation and influence changes to climate and weather patterns?  We'll answer this question in Part 4 of this series on the Last Interglacial......

0 0

Bookmark and Share Printable Version  |  Link to this page

Comments

Comments 1 to 18:

  1. Excellent posting!

    Expected rate of SLR?
    0 0
  2. How rapid was that SL fall?
    How rapid can the SL fall?
    0 0
  3. Minor point: "global sea-level is not the same everywhere and can vary by many metres from region to region"

    I thought measured ocean surface topography was on the order of 2 meters; most would say that 2 < many.



    Do the more recent data show more topography than this older satellite?
    0 0
  4. Paul - The Kopp et al paper I link to estimates a rate of 5-9 mm per year.


    muoncounter - you are totally correct if considering just stationary ocean surface topography. Local sea-level can temporarily be much greater than 2 m on a regional basis once you factor in waves and tides.
    0 0
  5. SteveB#4: "once you factor in waves and tides. "

    True enough. But even the tides are quoted as so many meters above mean sea level. Your 2nd paragraph gives me the impression that you are talking about this 'static' topography; essentially the shape of the geoid, to which we then add the transient wave and tidal ups and downs.

    Don't mind me; I took a GIS course this summer, so I'm all awash with datums and geoids.
    0 0
  6. Not really on-topic, but a bit related...

    I was musing on the notion that civilization has flourished in the current, steady interglacial, and wondered about human evolution during the last few ice ages cycles. Modern man evolved during a warm period (a degree or so cooler than present) about 200 000 years ago. Our species has survived two glacial maximums since. Is there any work in the literature linking temperate climate to evolutionary fecundity and/or increased biodiversity? Kind of opposite to the evidence of extinctions associated with 'rapid' climate change.
    0 0
  7. Barry,
    The extinction of megafauna at the end of the last ice age is thought (by those I read many years ago when I was an anthropology student) to be the main driver of the neolithic revolution. No longer being able to rely on following the herds of huge beasts, man was forced to exploit other food souces. Smaller tools were developed to hunt smaller prey including birds and fish.

    I cannot recall anything signifigant from the previous interglacial.
    You raise a good question. I'll look around and see if I can find anything for you.
    0 0
  8. Thanks, Stevo. I'll have a fossick too when I have a few hours to rub together.
    0 0
  9. An interesting post, though the question is perhaps how fast can sea level rise given the vulnerability of WAIS and the prospect of surging Arctic amplification?
    0 0
  10. Tom Curtis had an interesting comment under the "Where have all the people gone" post. Tom's assessment of the overall situation is very close to mine (that there will be bigger problems than coastal flooding), for whatever that's worth. However, Tom proposes that rates of rise in the past provide our best estimate of what can be expected out of the future, and my thought is that we don't know if the paleoclimate rates were constrained more by the physics of ice, or by the rate of warming of the planet at large. Since we are on a path of warming faster than before, if the former, then Tom is right, if the latter, we just don't know.

    If memory serves, a couple of years ago there was a study of the Greenland sheet that constrained how quickly ice can be lost based on how fast it can melt and how quickly ice can flow over the topography. This constrained sea level rise to 'only' 1-2 meters by 2100. On the Antarctic side, there is also this paper

    Stability of ice-sheet grounding lines

    and this news story based on it

    Major Antarctic glacier is 'past its tipping point'

    This is interesting to me because it factored in the model how an increase in sea level will accelerate the loss of ice from Antarctic, which will increase sea level. Without specifying a rate, it remains that the rise will accelerate.

    RealClimate has several posts which might be useful if you search for Greenland and WAIS, not at the same time necessarily.


    In agreement with the conclusion above, the evidence is building that Greenland is more stable than may have been thought 10 years ago, and the WAIS less stable.

    Agnostic,
    You will find varying estimates. A good start would be to Google Scholar "Stefan Rahmstorf", "Mauri Pelto", and others referenced in the links above. I don't think it matters that we know what the rate will be at any particular point in the future because, under BAU, it will accelerate until the supply of sheet ice to melt is reduced. That almost guarantees the rate will be more than we can easily cope with at some point, and it will be one problem of many.
    0 0
  11. Not to drone on, but let's put this in perspective. If we have a sea level rise of 1m by 2100, that is mostly an economic problem. If we have 4 K of warming by 2100... Well, by most accounts, that will present a challenge that is more than just economic.
    0 0
  12. OK, I am droning, but let me clarify something I wrote above. I don't think it matters too much in terms of if we should continue BAU, or in terms of mitigation strategies. It might still be significant in terms of planning for adaptation. Especially considering that we may have already lost most of the WAIS even if we do manage to stabilize temps a little higher than they are now.

    Probably it is also useful it getting the public to acknowledge that something needs to change, because I suspect that it is easier (not easy, just easier) to put error bounds around sea level rise than it is to put error bounds around crop production.
    0 0
  13. Barry #6,
    IDK, just because man has flourished does not mean that biodiversity has increased at the same time. From a certain distance, humans look like the most successful invasive species that has ever been. We are also a generalist species, and my impression is that generalists tend to do better than specialists during times of change.
    0 0
  14. just because man has flourished does not mean that biodiversity has increased at the same time


    I think you mistook my question for a statement. :-)

    I need more time in the day to look this stuff up.
    0 0
  15. Barry - There are papers suggesting that global biodiversity was diminished during "Greenhouse' periods. Contrary to James Inhofe's elementary school recollections of the time of the dinosaur.

    Such as this study: A long-term association between global temperature and biodiversity, origination and extinction in the fossil record - Mayhew (2007)

    Kinda makes sense for the marine environment. The oceans were uniformly warmer from pole-to-equator, and from the surface to deep ocean, therefore oxygen levels in the ocean would have been greatly reduced.
    0 0
  16. Bless you, Rob. Just the thing. Making time right now to read.
    0 0
  17. First skim - The tentative results are non-intuitive (to me), specifically regarding biodiversity at different temperatures. I would have thought that life would flourish more in a warmer (stable) global climate, like microbiological cultures in the lab, but the work indicates otherwise.

    Fascinating stuff. I'll re-read and follow up on the references. And I'll refrain from digressing here any further. Thanks for the allowance.
    0 0
  18. Mr. Chris G. pointed to a paper by Katz and Worster at
    http://rspa.royalsocietypublishing.org/content/466/2118/1597.full.pdf+html

    which I found fascinating. They do a 3-D calculation of the effect of a narrow retrograde valley embedded in a prograde slope under an ice sheet debouching to the ocean, and they find that such valleys can destabilize the entire ice sheet ! Also they find that PIG is melting faster than their model indicates...

    sidd
    0 0

You need to be logged in to post a comment. Login via the left margin or if you're new, register here.



The Consensus Project Website

TEXTBOOK

THE ESCALATOR

(free to republish)

THE DEBUNKING HANDBOOK

BOOK NOW AVAILABLE

The Scientific Guide to
Global Warming Skepticism

Smartphone Apps

iPhone
Android
Nokia

© Copyright 2014 John Cook
Home | Links | Translations | About Us | Contact Us