Extreme Translation Events of Atlantic Tropical Cyclones

Changes in the translational speed of tropical cyclones (e.g., sluggish tropical cyclones) are associated with extreme precipitation and flash flooding. However, it is still unclear regarding the spatial and temporal variability of extreme tropical cyclone translation events in the North Atlantic an...

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Published in:Atmosphere
Main Author: Wei Zhang
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12081032
https://doaj.org/article/74e6df25dd974c7689e576241c118042
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spelling ftdoajarticles:oai:doaj.org/article:74e6df25dd974c7689e576241c118042 2023-05-15T17:29:14+02:00 Extreme Translation Events of Atlantic Tropical Cyclones Wei Zhang 2021-08-01T00:00:00Z https://doi.org/10.3390/atmos12081032 https://doaj.org/article/74e6df25dd974c7689e576241c118042 EN eng MDPI AG https://www.mdpi.com/2073-4433/12/8/1032 https://doaj.org/toc/2073-4433 doi:10.3390/atmos12081032 2073-4433 https://doaj.org/article/74e6df25dd974c7689e576241c118042 Atmosphere, Vol 12, Iss 1032, p 1032 (2021) translation events tropical cyclones Atlantic extremes Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.3390/atmos12081032 2022-12-31T09:57:51Z Changes in the translational speed of tropical cyclones (e.g., sluggish tropical cyclones) are associated with extreme precipitation and flash flooding. However, it is still unclear regarding the spatial and temporal variability of extreme tropical cyclone translation events in the North Atlantic and underlying large-scale drivers. This work finds that the frequencies of extreme fast- and slow-translation events of Atlantic tropical cyclones exhibited a significant rising trend during 1980–2019. The extreme fast-translation events of Atlantic tropical cyclones are primarily located in the northern part of the North Atlantic, while the extreme slow-translation events are located more equatorward. There is a significant rising trend in the frequency of extreme slow-translation events over ocean with no trend over land. However, there is a significant rising trend in the frequency of extreme fast-translation events over ocean and over land. The extreme slow-translation events are associated with a strong high-pressure system in the continental United States (U.S.). By contrast, the extreme fast-translation events are related to a low-pressure system across most of the continental U.S. that leads to westerly steering flow that enhances tropical cyclone movement. This study suggests that it might be useful to separate tropical cyclone events into fast-moving and slow-moving groups when examining the translational speed of North Atlantic tropical cyclones, instead of examining regional or global mean translational speed. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Atmosphere 12 8 1032
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic translation events
tropical cyclones
Atlantic
extremes
Meteorology. Climatology
QC851-999
spellingShingle translation events
tropical cyclones
Atlantic
extremes
Meteorology. Climatology
QC851-999
Wei Zhang
Extreme Translation Events of Atlantic Tropical Cyclones
topic_facet translation events
tropical cyclones
Atlantic
extremes
Meteorology. Climatology
QC851-999
description Changes in the translational speed of tropical cyclones (e.g., sluggish tropical cyclones) are associated with extreme precipitation and flash flooding. However, it is still unclear regarding the spatial and temporal variability of extreme tropical cyclone translation events in the North Atlantic and underlying large-scale drivers. This work finds that the frequencies of extreme fast- and slow-translation events of Atlantic tropical cyclones exhibited a significant rising trend during 1980–2019. The extreme fast-translation events of Atlantic tropical cyclones are primarily located in the northern part of the North Atlantic, while the extreme slow-translation events are located more equatorward. There is a significant rising trend in the frequency of extreme slow-translation events over ocean with no trend over land. However, there is a significant rising trend in the frequency of extreme fast-translation events over ocean and over land. The extreme slow-translation events are associated with a strong high-pressure system in the continental United States (U.S.). By contrast, the extreme fast-translation events are related to a low-pressure system across most of the continental U.S. that leads to westerly steering flow that enhances tropical cyclone movement. This study suggests that it might be useful to separate tropical cyclone events into fast-moving and slow-moving groups when examining the translational speed of North Atlantic tropical cyclones, instead of examining regional or global mean translational speed.
format Article in Journal/Newspaper
author Wei Zhang
author_facet Wei Zhang
author_sort Wei Zhang
title Extreme Translation Events of Atlantic Tropical Cyclones
title_short Extreme Translation Events of Atlantic Tropical Cyclones
title_full Extreme Translation Events of Atlantic Tropical Cyclones
title_fullStr Extreme Translation Events of Atlantic Tropical Cyclones
title_full_unstemmed Extreme Translation Events of Atlantic Tropical Cyclones
title_sort extreme translation events of atlantic tropical cyclones
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/atmos12081032
https://doaj.org/article/74e6df25dd974c7689e576241c118042
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere, Vol 12, Iss 1032, p 1032 (2021)
op_relation https://www.mdpi.com/2073-4433/12/8/1032
https://doaj.org/toc/2073-4433
doi:10.3390/atmos12081032
2073-4433
https://doaj.org/article/74e6df25dd974c7689e576241c118042
op_doi https://doi.org/10.3390/atmos12081032
container_title Atmosphere
container_volume 12
container_issue 8
container_start_page 1032
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