Aspects of modern Antarctic meteorology and climatology
Great advances have been made in recent years in our understanding of the weather of the Antarctic and how the climate of the continent varies on a range of time-scales. The observations from the stations are still the most accurate meteorological measurements that we have, but satellites have been...
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2005
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Online Access: | http://dx.doi.org/10.3366/anh.2005.32.2.334 |
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credinunivpr:10.3366/anh.2005.32.2.334 2023-05-15T14:09:43+02:00 Aspects of modern Antarctic meteorology and climatology Turner, John 2005 http://dx.doi.org/10.3366/anh.2005.32.2.334 en eng Edinburgh University Press https://www.euppublishing.com/customer-services/librarians/text-and-data-mining-tdm Archives of Natural History volume 32, issue 2, page 334-345 ISSN 0260-9541 1755-6260 Agricultural and Biological Sciences (miscellaneous) History Anthropology journal-article 2005 credinunivpr https://doi.org/10.3366/anh.2005.32.2.334 2022-04-09T06:22:24Z Great advances have been made in recent years in our understanding of the weather of the Antarctic and how the climate of the continent varies on a range of time-scales. The observations from the stations are still the most accurate meteorological measurements that we have, but satellites have been important in providing data for remote parts of the continent and the Southern Ocean. With the large amount of data that is available today weather forecasts are much more accurate than just a few years ago and can provide valuable guidance up to several days ahead over the Southern Ocean and Antarctic coastal region. However, predicting the weather for the interior of the Antarctic is still very difficult. Recent research has shown that the climate of the Antarctic is affected by tropical atmospheric and oceanic climate cycles, such as the El Niño-Southern Oscillation, but the links are complex. The picture of climate change across the Antarctic during the last 50 years is complex, with only the Antarctic Peninsula showing a significant warming. By the end of the twenty-first century near-surface air temperatures across much of the Antarctic continent are expected to increase by several degrees. A small increase in precipitation is also expected. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Southern Ocean Edinburgh University Press (via Crossref) Antarctic Antarctic Peninsula Southern Ocean The Antarctic Archives of Natural History 32 2 334 345 |
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Open Polar |
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Edinburgh University Press (via Crossref) |
op_collection_id |
credinunivpr |
language |
English |
topic |
Agricultural and Biological Sciences (miscellaneous) History Anthropology |
spellingShingle |
Agricultural and Biological Sciences (miscellaneous) History Anthropology Turner, John Aspects of modern Antarctic meteorology and climatology |
topic_facet |
Agricultural and Biological Sciences (miscellaneous) History Anthropology |
description |
Great advances have been made in recent years in our understanding of the weather of the Antarctic and how the climate of the continent varies on a range of time-scales. The observations from the stations are still the most accurate meteorological measurements that we have, but satellites have been important in providing data for remote parts of the continent and the Southern Ocean. With the large amount of data that is available today weather forecasts are much more accurate than just a few years ago and can provide valuable guidance up to several days ahead over the Southern Ocean and Antarctic coastal region. However, predicting the weather for the interior of the Antarctic is still very difficult. Recent research has shown that the climate of the Antarctic is affected by tropical atmospheric and oceanic climate cycles, such as the El Niño-Southern Oscillation, but the links are complex. The picture of climate change across the Antarctic during the last 50 years is complex, with only the Antarctic Peninsula showing a significant warming. By the end of the twenty-first century near-surface air temperatures across much of the Antarctic continent are expected to increase by several degrees. A small increase in precipitation is also expected. |
format |
Article in Journal/Newspaper |
author |
Turner, John |
author_facet |
Turner, John |
author_sort |
Turner, John |
title |
Aspects of modern Antarctic meteorology and climatology |
title_short |
Aspects of modern Antarctic meteorology and climatology |
title_full |
Aspects of modern Antarctic meteorology and climatology |
title_fullStr |
Aspects of modern Antarctic meteorology and climatology |
title_full_unstemmed |
Aspects of modern Antarctic meteorology and climatology |
title_sort |
aspects of modern antarctic meteorology and climatology |
publisher |
Edinburgh University Press |
publishDate |
2005 |
url |
http://dx.doi.org/10.3366/anh.2005.32.2.334 |
geographic |
Antarctic Antarctic Peninsula Southern Ocean The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
op_source |
Archives of Natural History volume 32, issue 2, page 334-345 ISSN 0260-9541 1755-6260 |
op_rights |
https://www.euppublishing.com/customer-services/librarians/text-and-data-mining-tdm |
op_doi |
https://doi.org/10.3366/anh.2005.32.2.334 |
container_title |
Archives of Natural History |
container_volume |
32 |
container_issue |
2 |
container_start_page |
334 |
op_container_end_page |
345 |
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1766281736106278912 |