Weather whiplash: Trends in rapid temperature changes in a warming climate

Abstract Both research and media attention has shown an increasing interest in rapidly changing weather, colloquially termed “weather whiplash” events. This research examines the spatial and seasonal variability of trends in seasonally standardized short‐term temperature ranges across the globe. Tre...

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Published in:International Journal of Climatology
Main Author: Lee, Cameron C.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2021
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.7458
https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7458
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458
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spelling crwiley:10.1002/joc.7458 2024-06-02T08:02:32+00:00 Weather whiplash: Trends in rapid temperature changes in a warming climate Lee, Cameron C. 2021 http://dx.doi.org/10.1002/joc.7458 https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7458 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458 en eng Wiley http://creativecommons.org/licenses/by/4.0/ International Journal of Climatology volume 42, issue 8, page 4214-4222 ISSN 0899-8418 1097-0088 journal-article 2021 crwiley https://doi.org/10.1002/joc.7458 2024-05-03T11:25:36Z Abstract Both research and media attention has shown an increasing interest in rapidly changing weather, colloquially termed “weather whiplash” events. This research examines the spatial and seasonal variability of trends in seasonally standardized short‐term temperature ranges across the globe. Trends are calculated for three different “range windows”: 7‐day ranges, 1‐day departure, and diurnal (24‐hr) temperature ranges. Results show that globally, over the 70‐year period of record 7‐ and 1‐day ranges are increasing substantially in all seasons, while diurnal trends are only changing (decreasing) significantly in boreal autumn. Since 1985, however, ranges at all three time windows have increased significantly. The most widespread changes are occurring as significant increases in these ranges in the Southern Ocean, Africa, and South America and in regions of coastal upwelling. Significant decreases in these ranges are noted mostly at the Arctic Ocean confluence with the Pacific and Atlantic Oceans, especially in the Greenland, Iceland, and Norwegian Seas, and more recently, in northeastern Canada. Oceanic trends appear driven by changes in wind speeds, especially in the Southern Hemisphere where increasing open‐ocean winds are nearly ubiquitous. Trends in temperature variability over land are largely inverse of the long‐term changes in cloud cover. This research adds to a growing body of climate change literature examining temperature variability trends, and it represents the first examination of full 70‐year trends of many variables contained in the recently released ERA5 reanalysis. Article in Journal/Newspaper Arctic Arctic Ocean Climate change Greenland Iceland Southern Ocean Wiley Online Library Arctic Southern Ocean Arctic Ocean Canada Greenland Pacific International Journal of Climatology 42 8 4214 4222
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op_collection_id crwiley
language English
description Abstract Both research and media attention has shown an increasing interest in rapidly changing weather, colloquially termed “weather whiplash” events. This research examines the spatial and seasonal variability of trends in seasonally standardized short‐term temperature ranges across the globe. Trends are calculated for three different “range windows”: 7‐day ranges, 1‐day departure, and diurnal (24‐hr) temperature ranges. Results show that globally, over the 70‐year period of record 7‐ and 1‐day ranges are increasing substantially in all seasons, while diurnal trends are only changing (decreasing) significantly in boreal autumn. Since 1985, however, ranges at all three time windows have increased significantly. The most widespread changes are occurring as significant increases in these ranges in the Southern Ocean, Africa, and South America and in regions of coastal upwelling. Significant decreases in these ranges are noted mostly at the Arctic Ocean confluence with the Pacific and Atlantic Oceans, especially in the Greenland, Iceland, and Norwegian Seas, and more recently, in northeastern Canada. Oceanic trends appear driven by changes in wind speeds, especially in the Southern Hemisphere where increasing open‐ocean winds are nearly ubiquitous. Trends in temperature variability over land are largely inverse of the long‐term changes in cloud cover. This research adds to a growing body of climate change literature examining temperature variability trends, and it represents the first examination of full 70‐year trends of many variables contained in the recently released ERA5 reanalysis.
format Article in Journal/Newspaper
author Lee, Cameron C.
spellingShingle Lee, Cameron C.
Weather whiplash: Trends in rapid temperature changes in a warming climate
author_facet Lee, Cameron C.
author_sort Lee, Cameron C.
title Weather whiplash: Trends in rapid temperature changes in a warming climate
title_short Weather whiplash: Trends in rapid temperature changes in a warming climate
title_full Weather whiplash: Trends in rapid temperature changes in a warming climate
title_fullStr Weather whiplash: Trends in rapid temperature changes in a warming climate
title_full_unstemmed Weather whiplash: Trends in rapid temperature changes in a warming climate
title_sort weather whiplash: trends in rapid temperature changes in a warming climate
publisher Wiley
publishDate 2021
url http://dx.doi.org/10.1002/joc.7458
https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.7458
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.7458
geographic Arctic
Southern Ocean
Arctic Ocean
Canada
Greenland
Pacific
geographic_facet Arctic
Southern Ocean
Arctic Ocean
Canada
Greenland
Pacific
genre Arctic
Arctic Ocean
Climate change
Greenland
Iceland
Southern Ocean
genre_facet Arctic
Arctic Ocean
Climate change
Greenland
Iceland
Southern Ocean
op_source International Journal of Climatology
volume 42, issue 8, page 4214-4222
ISSN 0899-8418 1097-0088
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/joc.7458
container_title International Journal of Climatology
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