Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming.
The retreat of Antarctic ice sheets during the transition from the last glacial period to the Holocene provides the most recent example of ice sheet response to major climate forcing and thus allows rates of ice sheet decay and coupling to sea level rise to be quantified. We observe through a combin...
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ftansto:oai:apo-prod.ansto.gov.au:10238/2745 2023-05-15T13:36:16+02:00 Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. Mackintosh, AN Domack, E Golledge, NR Dunbar, R Leventer, A White, D Fink, D Gore, DB Lavoie, C 2009-07-01 http://apo.ansto.gov.au/dspace/handle/10238/2745 en eng Mackintosh, A., Domack, E., Golledge, N., Dunbar, R., Leventer, A., White, D., Fink, D., Gore, D., & Lavoie, C. (2009). Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. Annual Antarctic Conference 2009 - "Sustaining the Gains of the International Polar Year", 1st – 3rd July 2009. In Proceedings of the Annual Antarctic Conference 2009 (p. 13). Auckland, New Zealand: University of Auckland. 1176-5798 http://apo.ansto.gov.au/dspace/handle/10238/2745 Antarctica Ice Quaternary period Sea level Greenhouse effect Climatic change Conference Presentation 2009 ftansto 2020-08-03T22:28:23Z The retreat of Antarctic ice sheets during the transition from the last glacial period to the Holocene provides the most recent example of ice sheet response to major climate forcing and thus allows rates of ice sheet decay and coupling to sea level rise to be quantified. We observe through a combination of land- and marine-based geochronology and ice sheet modelling, a highly-resolved temporal record of deglaciation of the East Antarctic Ice Sheet across the Mac.Robertson Land shelf. Our reconstruction demonstrates that deglaciation of deep-shelf troughs and lowering of the ice sheet surface occurred in two phases, from 14 - 12 and 12 - 7 ka before present (BP). Our consideration of possible mechanisms for the observed retreat of the marine ice margin of Mac.Robertson Land favours rapid rates of eustatic sea level rise associated with Meltwater Pulse 1a (MWP-1a) at ~14 ka BP and warming of the marginal oceans and atmosphere to nearmodern levels ~2 ka later. In support of this interpretation is the comparison of our land-marine sequence to other well-constrained marine deglacial events from both West and East Antarctica, including the Ross and Weddell Sea embayments. Our results show that periods of rapid sea level rise can initiate instability in Antarctica’s ice masses, including the margins of East Antarctica, and indicate that a combination of sea level rise and oceanic warming is a powerful driver of ice retreat. Conference Object Antarc* Antarctic Antarctica East Antarctica Ice Sheet Mac.Robertson Land Weddell Sea Australian Nuclear Science and Technology Organisation: ANSTO Publications Online Antarctic East Antarctic Ice Sheet East Antarctica Mac.Robertson Land ENVELOPE(65.000,65.000,-70.000,-70.000) Weddell Weddell Sea |
institution |
Open Polar |
collection |
Australian Nuclear Science and Technology Organisation: ANSTO Publications Online |
op_collection_id |
ftansto |
language |
English |
topic |
Antarctica Ice Quaternary period Sea level Greenhouse effect Climatic change |
spellingShingle |
Antarctica Ice Quaternary period Sea level Greenhouse effect Climatic change Mackintosh, AN Domack, E Golledge, NR Dunbar, R Leventer, A White, D Fink, D Gore, DB Lavoie, C Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
topic_facet |
Antarctica Ice Quaternary period Sea level Greenhouse effect Climatic change |
description |
The retreat of Antarctic ice sheets during the transition from the last glacial period to the Holocene provides the most recent example of ice sheet response to major climate forcing and thus allows rates of ice sheet decay and coupling to sea level rise to be quantified. We observe through a combination of land- and marine-based geochronology and ice sheet modelling, a highly-resolved temporal record of deglaciation of the East Antarctic Ice Sheet across the Mac.Robertson Land shelf. Our reconstruction demonstrates that deglaciation of deep-shelf troughs and lowering of the ice sheet surface occurred in two phases, from 14 - 12 and 12 - 7 ka before present (BP). Our consideration of possible mechanisms for the observed retreat of the marine ice margin of Mac.Robertson Land favours rapid rates of eustatic sea level rise associated with Meltwater Pulse 1a (MWP-1a) at ~14 ka BP and warming of the marginal oceans and atmosphere to nearmodern levels ~2 ka later. In support of this interpretation is the comparison of our land-marine sequence to other well-constrained marine deglacial events from both West and East Antarctica, including the Ross and Weddell Sea embayments. Our results show that periods of rapid sea level rise can initiate instability in Antarctica’s ice masses, including the margins of East Antarctica, and indicate that a combination of sea level rise and oceanic warming is a powerful driver of ice retreat. |
format |
Conference Object |
author |
Mackintosh, AN Domack, E Golledge, NR Dunbar, R Leventer, A White, D Fink, D Gore, DB Lavoie, C |
author_facet |
Mackintosh, AN Domack, E Golledge, NR Dunbar, R Leventer, A White, D Fink, D Gore, DB Lavoie, C |
author_sort |
Mackintosh, AN |
title |
Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
title_short |
Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
title_full |
Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
title_fullStr |
Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
title_full_unstemmed |
Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. |
title_sort |
last major retreat of antarctic ice sheets forced by sea level rise and ocean warming. |
publishDate |
2009 |
url |
http://apo.ansto.gov.au/dspace/handle/10238/2745 |
long_lat |
ENVELOPE(65.000,65.000,-70.000,-70.000) |
geographic |
Antarctic East Antarctic Ice Sheet East Antarctica Mac.Robertson Land Weddell Weddell Sea |
geographic_facet |
Antarctic East Antarctic Ice Sheet East Antarctica Mac.Robertson Land Weddell Weddell Sea |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Mac.Robertson Land Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Mac.Robertson Land Weddell Sea |
op_relation |
Mackintosh, A., Domack, E., Golledge, N., Dunbar, R., Leventer, A., White, D., Fink, D., Gore, D., & Lavoie, C. (2009). Last major retreat of Antarctic ice sheets forced by sea level rise and ocean warming. Annual Antarctic Conference 2009 - "Sustaining the Gains of the International Polar Year", 1st – 3rd July 2009. In Proceedings of the Annual Antarctic Conference 2009 (p. 13). Auckland, New Zealand: University of Auckland. 1176-5798 http://apo.ansto.gov.au/dspace/handle/10238/2745 |
_version_ |
1766076295197753344 |