Winter climate change on the northern and southern Antarctic Peninsula
Abstract Differences in the decadal trend in the winter surface temperature in the northern and southern Antarctic Peninsula have been analysed. Time series from the two stations Esperanza and Faraday/Vernadsky since the early 1950s are used. The two time series are strongly correlated only during t...
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Online Access: | http://dx.doi.org/10.1017/s0954102020000255 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102020000255 |
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crcambridgeupr:10.1017/s0954102020000255 2024-04-28T07:59:46+00:00 Winter climate change on the northern and southern Antarctic Peninsula Evtushevsky, Oleksandr M. Kravchenko, Volodymyr O. Grytsai, Asen V. Milinevsky, Gennadi P. 2020 http://dx.doi.org/10.1017/s0954102020000255 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102020000255 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 32, issue 5, page 408-424 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2020 crcambridgeupr https://doi.org/10.1017/s0954102020000255 2024-04-09T06:55:37Z Abstract Differences in the decadal trend in the winter surface temperature in the northern and southern Antarctic Peninsula have been analysed. Time series from the two stations Esperanza and Faraday/Vernadsky since the early 1950s are used. The two time series are strongly correlated only during the 1980s and 1990s when their variability and trends are associated with both the Niño-4 region and Southern Annular Mode impacts. The winter cooling at the Faraday/Vernadsky station contrasts with the winter warming at the Esperanza station during the period of 2006–17. The different temperature trends are accompanied by weak correlations between the temperatures at these two stations. Linearly congruent components of the station temperature trends in 2006–17 indicate a dominant contribution of Southern Annular Mode (tropical sea surface temperature anomalies) to warming (cooling) in the northern (southern) Peninsula. Distinctive impacts of climate modes are observed in combination with the recent deepening of the negative sea-level pressure anomaly to the west of the peninsula and the related change in the zonal and meridional wind components. These factors apparently contribute to the occurrence of the boundary that crosses the peninsula and divides it into sub-regions with warming and cooling. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctic Science Cambridge University Press Antarctic Science 32 5 408 424 |
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Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
spellingShingle |
Geology Ecology, Evolution, Behavior and Systematics Oceanography Evtushevsky, Oleksandr M. Kravchenko, Volodymyr O. Grytsai, Asen V. Milinevsky, Gennadi P. Winter climate change on the northern and southern Antarctic Peninsula |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Abstract Differences in the decadal trend in the winter surface temperature in the northern and southern Antarctic Peninsula have been analysed. Time series from the two stations Esperanza and Faraday/Vernadsky since the early 1950s are used. The two time series are strongly correlated only during the 1980s and 1990s when their variability and trends are associated with both the Niño-4 region and Southern Annular Mode impacts. The winter cooling at the Faraday/Vernadsky station contrasts with the winter warming at the Esperanza station during the period of 2006–17. The different temperature trends are accompanied by weak correlations between the temperatures at these two stations. Linearly congruent components of the station temperature trends in 2006–17 indicate a dominant contribution of Southern Annular Mode (tropical sea surface temperature anomalies) to warming (cooling) in the northern (southern) Peninsula. Distinctive impacts of climate modes are observed in combination with the recent deepening of the negative sea-level pressure anomaly to the west of the peninsula and the related change in the zonal and meridional wind components. These factors apparently contribute to the occurrence of the boundary that crosses the peninsula and divides it into sub-regions with warming and cooling. |
format |
Article in Journal/Newspaper |
author |
Evtushevsky, Oleksandr M. Kravchenko, Volodymyr O. Grytsai, Asen V. Milinevsky, Gennadi P. |
author_facet |
Evtushevsky, Oleksandr M. Kravchenko, Volodymyr O. Grytsai, Asen V. Milinevsky, Gennadi P. |
author_sort |
Evtushevsky, Oleksandr M. |
title |
Winter climate change on the northern and southern Antarctic Peninsula |
title_short |
Winter climate change on the northern and southern Antarctic Peninsula |
title_full |
Winter climate change on the northern and southern Antarctic Peninsula |
title_fullStr |
Winter climate change on the northern and southern Antarctic Peninsula |
title_full_unstemmed |
Winter climate change on the northern and southern Antarctic Peninsula |
title_sort |
winter climate change on the northern and southern antarctic peninsula |
publisher |
Cambridge University Press (CUP) |
publishDate |
2020 |
url |
http://dx.doi.org/10.1017/s0954102020000255 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102020000255 |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctic Science |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctic Science |
op_source |
Antarctic Science volume 32, issue 5, page 408-424 ISSN 0954-1020 1365-2079 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0954102020000255 |
container_title |
Antarctic Science |
container_volume |
32 |
container_issue |
5 |
container_start_page |
408 |
op_container_end_page |
424 |
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1797572315591999488 |