Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate
Quantitative estimates of future Antarctic climate change are derived from numerical global climate models. Evaluation of the reliability of climate model projections involves many lines of evidence on past performance combined with knowledge of the processes that need to be represented. Routine mod...
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ftmdpi:oai:mdpi.com:/2076-3263/9/6/255/ 2023-08-20T04:01:11+02:00 Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate Thomas J. Bracegirdle Florence Colleoni Nerilie J. Abram Nancy A. N. Bertler Daniel A. Dixon Mark England Vincent Favier Chris J. Fogwill John C. Fyfe Ian Goodwin Hugues Goosse Will Hobbs Julie M. Jones Elizabeth D. Keller Alia L. Khan Steven J. Phipps Marilyn N. Raphael Joellen Russell Louise Sime Elizabeth R. Thomas Michiel R. van den Broeke Ilana Wainer agris 2019-06-07 application/pdf https://doi.org/10.3390/geosciences9060255 EN eng Multidisciplinary Digital Publishing Institute Geophysics https://dx.doi.org/10.3390/geosciences9060255 https://creativecommons.org/licenses/by/4.0/ Geosciences; Volume 9; Issue 6; Pages: 255 Antarctic Southern Ocean climate paleoclimate CMIP PMIP projections Text 2019 ftmdpi https://doi.org/10.3390/geosciences9060255 2023-07-31T22:20:32Z Quantitative estimates of future Antarctic climate change are derived from numerical global climate models. Evaluation of the reliability of climate model projections involves many lines of evidence on past performance combined with knowledge of the processes that need to be represented. Routine model evaluation is mainly based on the modern observational period, which started with the establishment of a network of Antarctic weather stations in 1957/58. This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends. To help address this gap, we present a new evaluation of potential ways in which long-term observational and paleo-proxy reconstructions may be used, with a particular focus on improving projections. A wide range of data sources and time periods is included, ranging from ship observations of the early 20th century to ice core records spanning hundreds to hundreds of thousands of years to sediment records dating back 34 million years. We conclude that paleo-proxy records and long-term observational datasets are an underused resource in terms of strategies for improving Antarctic climate projections for the 21st century and beyond. We identify priorities and suggest next steps to addressing this. Text Antarc* Antarctic ice core Southern Ocean MDPI Open Access Publishing Antarctic Southern Ocean The Antarctic Geosciences 9 6 255 |
institution |
Open Polar |
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MDPI Open Access Publishing |
op_collection_id |
ftmdpi |
language |
English |
topic |
Antarctic Southern Ocean climate paleoclimate CMIP PMIP projections |
spellingShingle |
Antarctic Southern Ocean climate paleoclimate CMIP PMIP projections Thomas J. Bracegirdle Florence Colleoni Nerilie J. Abram Nancy A. N. Bertler Daniel A. Dixon Mark England Vincent Favier Chris J. Fogwill John C. Fyfe Ian Goodwin Hugues Goosse Will Hobbs Julie M. Jones Elizabeth D. Keller Alia L. Khan Steven J. Phipps Marilyn N. Raphael Joellen Russell Louise Sime Elizabeth R. Thomas Michiel R. van den Broeke Ilana Wainer Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
topic_facet |
Antarctic Southern Ocean climate paleoclimate CMIP PMIP projections |
description |
Quantitative estimates of future Antarctic climate change are derived from numerical global climate models. Evaluation of the reliability of climate model projections involves many lines of evidence on past performance combined with knowledge of the processes that need to be represented. Routine model evaluation is mainly based on the modern observational period, which started with the establishment of a network of Antarctic weather stations in 1957/58. This period is too short to evaluate many fundamental aspects of the Antarctic and Southern Ocean climate system, such as decadal-to-century time-scale climate variability and trends. To help address this gap, we present a new evaluation of potential ways in which long-term observational and paleo-proxy reconstructions may be used, with a particular focus on improving projections. A wide range of data sources and time periods is included, ranging from ship observations of the early 20th century to ice core records spanning hundreds to hundreds of thousands of years to sediment records dating back 34 million years. We conclude that paleo-proxy records and long-term observational datasets are an underused resource in terms of strategies for improving Antarctic climate projections for the 21st century and beyond. We identify priorities and suggest next steps to addressing this. |
format |
Text |
author |
Thomas J. Bracegirdle Florence Colleoni Nerilie J. Abram Nancy A. N. Bertler Daniel A. Dixon Mark England Vincent Favier Chris J. Fogwill John C. Fyfe Ian Goodwin Hugues Goosse Will Hobbs Julie M. Jones Elizabeth D. Keller Alia L. Khan Steven J. Phipps Marilyn N. Raphael Joellen Russell Louise Sime Elizabeth R. Thomas Michiel R. van den Broeke Ilana Wainer |
author_facet |
Thomas J. Bracegirdle Florence Colleoni Nerilie J. Abram Nancy A. N. Bertler Daniel A. Dixon Mark England Vincent Favier Chris J. Fogwill John C. Fyfe Ian Goodwin Hugues Goosse Will Hobbs Julie M. Jones Elizabeth D. Keller Alia L. Khan Steven J. Phipps Marilyn N. Raphael Joellen Russell Louise Sime Elizabeth R. Thomas Michiel R. van den Broeke Ilana Wainer |
author_sort |
Thomas J. Bracegirdle |
title |
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
title_short |
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
title_full |
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
title_fullStr |
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
title_full_unstemmed |
Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate |
title_sort |
back to the future: using long-term observational and paleo-proxy reconstructions to improve model projections of antarctic climate |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2019 |
url |
https://doi.org/10.3390/geosciences9060255 |
op_coverage |
agris |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic ice core Southern Ocean |
genre_facet |
Antarc* Antarctic ice core Southern Ocean |
op_source |
Geosciences; Volume 9; Issue 6; Pages: 255 |
op_relation |
Geophysics https://dx.doi.org/10.3390/geosciences9060255 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/geosciences9060255 |
container_title |
Geosciences |
container_volume |
9 |
container_issue |
6 |
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255 |
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1774723283235635200 |