Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’
The Antarctic region has profoundly affected the global climates of the Cenozoic, influencing sea levels, atmospheric composition and dynamics, and ocean circulation. According to IPCC-2007 (IPCC, 2007) worst-case scenario projections, temperatures by 2100 are likely to exceed those that have been e...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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Online Access: | http://hdl.handle.net/2122/3394 https://doi.org/10.1016/j.palaeo.2007.12.001 |
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ftingv:oai:www.earth-prints.org:2122/3394 2023-05-15T13:51:39+02:00 Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ Florindo, F. Nelson, A. E. Haywood, A. M. Florindo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Nelson, A. E.; British Antarctic Survey, High Cross, Madingley Road, CB3 0ET, Cambridge, UK Haywood, A. M.; School of Earth and Environment, University of Leeds, LS2 9JT, UK Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia British Antarctic Survey, High Cross, Madingley Road, CB3 0ET, Cambridge, UK School of Earth and Environment, University of Leeds, LS2 9JT, UK 2007 http://hdl.handle.net/2122/3394 https://doi.org/10.1016/j.palaeo.2007.12.001 en eng Palaeogeography, Palaeoclimatology, Palaeoecology http://hdl.handle.net/2122/3394 doi:10.1016/j.palaeo.2007.12.001 restricted Antarctica Cenozoic 02. Cryosphere::02.04. Sea ice::02.04.99. General or miscellaneous 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous manuscript 2007 ftingv https://doi.org/10.1016/j.palaeo.2007.12.001 2022-07-29T06:04:46Z The Antarctic region has profoundly affected the global climates of the Cenozoic, influencing sea levels, atmospheric composition and dynamics, and ocean circulation. According to IPCC-2007 (IPCC, 2007) worst-case scenario projections, temperatures by 2100 are likely to exceed those that have been experienced by the Earth in the last 40 myr when the Antarctic Ice Sheet may have first developed. This implies that the Ice Sheet will become unsustainable, with huge implications for global sea-levels. In press 2.2. Laboratorio di paleomagnetismo JCR Journal reserved Manuscript Antarc* Antarctic Antarctica Ice Sheet Sea ice Southern Ocean Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Antarctic Southern Ocean The Antarctic Palaeogeography, Palaeoclimatology, Palaeoecology 260 1-2 1 7 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Antarctica Cenozoic 02. Cryosphere::02.04. Sea ice::02.04.99. General or miscellaneous 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous |
spellingShingle |
Antarctica Cenozoic 02. Cryosphere::02.04. Sea ice::02.04.99. General or miscellaneous 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous Florindo, F. Nelson, A. E. Haywood, A. M. Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
topic_facet |
Antarctica Cenozoic 02. Cryosphere::02.04. Sea ice::02.04.99. General or miscellaneous 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous |
description |
The Antarctic region has profoundly affected the global climates of the Cenozoic, influencing sea levels, atmospheric composition and dynamics, and ocean circulation. According to IPCC-2007 (IPCC, 2007) worst-case scenario projections, temperatures by 2100 are likely to exceed those that have been experienced by the Earth in the last 40 myr when the Antarctic Ice Sheet may have first developed. This implies that the Ice Sheet will become unsustainable, with huge implications for global sea-levels. In press 2.2. Laboratorio di paleomagnetismo JCR Journal reserved |
author2 |
Florindo, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Nelson, A. E.; British Antarctic Survey, High Cross, Madingley Road, CB3 0ET, Cambridge, UK Haywood, A. M.; School of Earth and Environment, University of Leeds, LS2 9JT, UK Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia British Antarctic Survey, High Cross, Madingley Road, CB3 0ET, Cambridge, UK School of Earth and Environment, University of Leeds, LS2 9JT, UK |
format |
Manuscript |
author |
Florindo, F. Nelson, A. E. Haywood, A. M. |
author_facet |
Florindo, F. Nelson, A. E. Haywood, A. M. |
author_sort |
Florindo, F. |
title |
Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
title_short |
Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
title_full |
Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
title_fullStr |
Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
title_full_unstemmed |
Introduction to ‘Antarctic cryosphere and Southern Ocean climate evolution (Cenozoic-Holocene)’ |
title_sort |
introduction to ‘antarctic cryosphere and southern ocean climate evolution (cenozoic-holocene)’ |
publishDate |
2007 |
url |
http://hdl.handle.net/2122/3394 https://doi.org/10.1016/j.palaeo.2007.12.001 |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Sea ice Southern Ocean |
op_relation |
Palaeogeography, Palaeoclimatology, Palaeoecology http://hdl.handle.net/2122/3394 doi:10.1016/j.palaeo.2007.12.001 |
op_rights |
restricted |
op_doi |
https://doi.org/10.1016/j.palaeo.2007.12.001 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
260 |
container_issue |
1-2 |
container_start_page |
1 |
op_container_end_page |
7 |
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1766255652567515136 |