Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores?
Measurements of Last Interglacial stable water isotopes in ice cores show that central Greenland δ18O increased by at least 3‰ compared to present day. Attempting to quantify the Greenland interglacial temperature change from these ice core measurements rests on our ability to interpret the stable w...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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2013
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Online Access: | http://eprints.esc.cam.ac.uk/2806/ http://eprints.esc.cam.ac.uk/2806/1/1-s2.0-S0277379113000188-main.pdf http://eprints.esc.cam.ac.uk/2806/2/1-s2.0-S0277379113000188-gr1.jpg http://www.sciencedirect.com/science/article/pii/S0277379113000188 https://doi.org/10.1016/j.quascirev.2013.01.009 |
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:2806 |
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Open Polar |
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University of Cambridge, Department of Earth Sciences: ESC Publications |
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ftucambridgeesc |
language |
English |
topic |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
spellingShingle |
01 - Climate Change and Earth-Ocean Atmosphere Systems Sime, L.C. Risi, C. Tindall, J.C. Sjolte, J. Wolff, E. W. Masson-Delmotte, V. Capron, E. Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
Measurements of Last Interglacial stable water isotopes in ice cores show that central Greenland δ18O increased by at least 3‰ compared to present day. Attempting to quantify the Greenland interglacial temperature change from these ice core measurements rests on our ability to interpret the stable water isotope content of Greenland snow. Current orbitally driven interglacial simulations do not show δ18O or temperature rises of the correct magnitude, leading to difficulty in using only these experiments to inform our understanding of higher interglacial δ18O. Here, analysis of greenhouse gas warmed simulations from two isotope-enabled general circulation models, in conjunction with a set of Last Interglacial sea surface observations, indicates a possible explanation for the interglacial δ18O rise. A reduction in the winter time sea ice concentration around the northern half of Greenland, together with an increase in sea surface temperatures over the same region, is found to be sufficient to drive a >3‰ interglacial enrichment in central Greenland snow. Warm climate δ18O and δD in precipitation falling on Greenland are shown to be strongly influenced by local sea surface condition changes: local sea surface warming and a shrunken sea ice extent increase the proportion of water vapour from local (isotopically enriched) sources, compared to that from distal (isotopically depleted) sources. Precipitation intermittency changes, under warmer conditions, leads to geographical variability in the δ18O against temperature gradients across Greenland. Little sea surface warming around the northern areas of Greenland leads to low δ18O against temperature gradients (0.1–0.3‰ per °C), whilst large sea surface warmings in these regions leads to higher gradients (0.3–0.7‰ per °C). These gradients imply a wide possible range of present day to interglacial temperature increases (4 to >10 °C). Thus, we find that uncertainty about local interglacial sea surface conditions, rather than precipitation intermittency changes, may lead to the largest uncertainties in interpreting temperature from Greenland ice cores. We find that interglacial sea surface change observational records are currently insufficient to enable discrimination between these different δ18O against temperature gradients. In conclusion, further information on interglacial sea surface temperatures and sea ice changes around northern Greenland should indicate whether +5 °C during the Last Interglacial is sufficient to drive the observed ice core δ18O increase, or whether a larger temperature increases or ice sheet changes are also required to explain the ice core observations. |
format |
Article in Journal/Newspaper |
author |
Sime, L.C. Risi, C. Tindall, J.C. Sjolte, J. Wolff, E. W. Masson-Delmotte, V. Capron, E. |
author_facet |
Sime, L.C. Risi, C. Tindall, J.C. Sjolte, J. Wolff, E. W. Masson-Delmotte, V. Capron, E. |
author_sort |
Sime, L.C. |
title |
Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
title_short |
Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
title_full |
Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
title_fullStr |
Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
title_full_unstemmed |
Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? |
title_sort |
warm climate isotopic simulations: what do we learn about interglacial signals in greenland ice cores? |
publishDate |
2013 |
url |
http://eprints.esc.cam.ac.uk/2806/ http://eprints.esc.cam.ac.uk/2806/1/1-s2.0-S0277379113000188-main.pdf http://eprints.esc.cam.ac.uk/2806/2/1-s2.0-S0277379113000188-gr1.jpg http://www.sciencedirect.com/science/article/pii/S0277379113000188 https://doi.org/10.1016/j.quascirev.2013.01.009 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice cores ice core Ice Sheet Sea ice |
genre_facet |
Greenland Greenland ice cores ice core Ice Sheet Sea ice |
op_relation |
http://eprints.esc.cam.ac.uk/2806/1/1-s2.0-S0277379113000188-main.pdf http://eprints.esc.cam.ac.uk/2806/2/1-s2.0-S0277379113000188-gr1.jpg Sime, L.C. and Risi, C. and Tindall, J.C. and Sjolte, J. and Wolff, E. W. and Masson-Delmotte, V. and Capron, E. (2013) Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? Quaternary Science Reviews, 67. pp. 59-80. ISSN 0277-3791 DOI https://doi.org/10.1016/j.quascirev.2013.01.009 <https://doi.org/10.1016/j.quascirev.2013.01.009> |
op_doi |
https://doi.org/10.1016/j.quascirev.2013.01.009 |
container_title |
Quaternary Science Reviews |
container_volume |
67 |
container_start_page |
59 |
op_container_end_page |
80 |
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1766012357661687808 |
spelling |
ftucambridgeesc:oai:eprints.esc.cam.ac.uk:2806 2023-05-15T16:23:59+02:00 Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? Sime, L.C. Risi, C. Tindall, J.C. Sjolte, J. Wolff, E. W. Masson-Delmotte, V. Capron, E. 2013-05 text image http://eprints.esc.cam.ac.uk/2806/ http://eprints.esc.cam.ac.uk/2806/1/1-s2.0-S0277379113000188-main.pdf http://eprints.esc.cam.ac.uk/2806/2/1-s2.0-S0277379113000188-gr1.jpg http://www.sciencedirect.com/science/article/pii/S0277379113000188 https://doi.org/10.1016/j.quascirev.2013.01.009 en eng http://eprints.esc.cam.ac.uk/2806/1/1-s2.0-S0277379113000188-main.pdf http://eprints.esc.cam.ac.uk/2806/2/1-s2.0-S0277379113000188-gr1.jpg Sime, L.C. and Risi, C. and Tindall, J.C. and Sjolte, J. and Wolff, E. W. and Masson-Delmotte, V. and Capron, E. (2013) Warm climate isotopic simulations: what do we learn about interglacial signals in Greenland ice cores? Quaternary Science Reviews, 67. pp. 59-80. ISSN 0277-3791 DOI https://doi.org/10.1016/j.quascirev.2013.01.009 <https://doi.org/10.1016/j.quascirev.2013.01.009> 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2013 ftucambridgeesc https://doi.org/10.1016/j.quascirev.2013.01.009 2020-08-27T18:09:24Z Measurements of Last Interglacial stable water isotopes in ice cores show that central Greenland δ18O increased by at least 3‰ compared to present day. Attempting to quantify the Greenland interglacial temperature change from these ice core measurements rests on our ability to interpret the stable water isotope content of Greenland snow. Current orbitally driven interglacial simulations do not show δ18O or temperature rises of the correct magnitude, leading to difficulty in using only these experiments to inform our understanding of higher interglacial δ18O. Here, analysis of greenhouse gas warmed simulations from two isotope-enabled general circulation models, in conjunction with a set of Last Interglacial sea surface observations, indicates a possible explanation for the interglacial δ18O rise. A reduction in the winter time sea ice concentration around the northern half of Greenland, together with an increase in sea surface temperatures over the same region, is found to be sufficient to drive a >3‰ interglacial enrichment in central Greenland snow. Warm climate δ18O and δD in precipitation falling on Greenland are shown to be strongly influenced by local sea surface condition changes: local sea surface warming and a shrunken sea ice extent increase the proportion of water vapour from local (isotopically enriched) sources, compared to that from distal (isotopically depleted) sources. Precipitation intermittency changes, under warmer conditions, leads to geographical variability in the δ18O against temperature gradients across Greenland. Little sea surface warming around the northern areas of Greenland leads to low δ18O against temperature gradients (0.1–0.3‰ per °C), whilst large sea surface warmings in these regions leads to higher gradients (0.3–0.7‰ per °C). These gradients imply a wide possible range of present day to interglacial temperature increases (4 to >10 °C). Thus, we find that uncertainty about local interglacial sea surface conditions, rather than precipitation intermittency changes, may lead to the largest uncertainties in interpreting temperature from Greenland ice cores. We find that interglacial sea surface change observational records are currently insufficient to enable discrimination between these different δ18O against temperature gradients. In conclusion, further information on interglacial sea surface temperatures and sea ice changes around northern Greenland should indicate whether +5 °C during the Last Interglacial is sufficient to drive the observed ice core δ18O increase, or whether a larger temperature increases or ice sheet changes are also required to explain the ice core observations. Article in Journal/Newspaper Greenland Greenland ice cores ice core Ice Sheet Sea ice University of Cambridge, Department of Earth Sciences: ESC Publications Greenland Quaternary Science Reviews 67 59 80 |