Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones

The climatology of tropical cyclones is an immediate research need, specifically to better understand their long-term patterns and elucidate their future in a changing climate. One important pattern that has recently been detected is the poleward shift of the lifetime maximum intensity (LMI) of trop...

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Published in:Atmosphere
Main Authors: Sarah A. Tennille, Kelsey N. Ellis
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2017
Subjects:
Online Access:https://doi.org/10.3390/atmos8100198
https://doaj.org/article/d11c933b63a84e3486f77c51fc5be2ff
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spelling ftdoajarticles:oai:doaj.org/article:d11c933b63a84e3486f77c51fc5be2ff 2023-05-15T17:29:13+02:00 Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones Sarah A. Tennille Kelsey N. Ellis 2017-10-01T00:00:00Z https://doi.org/10.3390/atmos8100198 https://doaj.org/article/d11c933b63a84e3486f77c51fc5be2ff EN eng MDPI AG https://www.mdpi.com/2073-4433/8/10/198 https://doaj.org/toc/2073-4433 2073-4433 doi:10.3390/atmos8100198 https://doaj.org/article/d11c933b63a84e3486f77c51fc5be2ff Atmosphere, Vol 8, Iss 10, p 198 (2017) hurricane maximum intensity wind speed climate change Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.3390/atmos8100198 2022-12-30T21:32:51Z The climatology of tropical cyclones is an immediate research need, specifically to better understand their long-term patterns and elucidate their future in a changing climate. One important pattern that has recently been detected is the poleward shift of the lifetime maximum intensity (LMI) of tropical cyclones. This study further assessed the recent (1977–2015) spatial changes in the LMI of tropical cyclones, specifically those of tropical storm strength or stronger in the North Atlantic and northern West Pacific basins. Analyses of moving decadal means suggested that LMI locations migrated south in the North Atlantic and north in the West Pacific. In addition to a linear trend, there is a cyclical migration of LMI that is especially apparent in the West Pacific. Relationships between LMI migration and intensity were explored, as well as LMI location relative to landfall. The southerly trend of LMI in the North Atlantic was most prevalent in the strongest storms, resulting in these storms reaching their LMI farther from land. The relationship between intensity and LMI migration in the West Pacific was not as clear, but the most intense storms have been reaching LMI closer to their eventual landfall location. This work adds to those emphasizing the importance of understanding the climatology of the most intense hurricanes and shows there are potential human impacts resulting from any migration of LMI. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Atmosphere 8 12 198
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic hurricane
maximum intensity
wind speed
climate change
Meteorology. Climatology
QC851-999
spellingShingle hurricane
maximum intensity
wind speed
climate change
Meteorology. Climatology
QC851-999
Sarah A. Tennille
Kelsey N. Ellis
Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
topic_facet hurricane
maximum intensity
wind speed
climate change
Meteorology. Climatology
QC851-999
description The climatology of tropical cyclones is an immediate research need, specifically to better understand their long-term patterns and elucidate their future in a changing climate. One important pattern that has recently been detected is the poleward shift of the lifetime maximum intensity (LMI) of tropical cyclones. This study further assessed the recent (1977–2015) spatial changes in the LMI of tropical cyclones, specifically those of tropical storm strength or stronger in the North Atlantic and northern West Pacific basins. Analyses of moving decadal means suggested that LMI locations migrated south in the North Atlantic and north in the West Pacific. In addition to a linear trend, there is a cyclical migration of LMI that is especially apparent in the West Pacific. Relationships between LMI migration and intensity were explored, as well as LMI location relative to landfall. The southerly trend of LMI in the North Atlantic was most prevalent in the strongest storms, resulting in these storms reaching their LMI farther from land. The relationship between intensity and LMI migration in the West Pacific was not as clear, but the most intense storms have been reaching LMI closer to their eventual landfall location. This work adds to those emphasizing the importance of understanding the climatology of the most intense hurricanes and shows there are potential human impacts resulting from any migration of LMI.
format Article in Journal/Newspaper
author Sarah A. Tennille
Kelsey N. Ellis
author_facet Sarah A. Tennille
Kelsey N. Ellis
author_sort Sarah A. Tennille
title Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
title_short Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
title_full Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
title_fullStr Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
title_full_unstemmed Spatial and Temporal Trends in the Location of the Lifetime Maximum Intensity of Tropical Cyclones
title_sort spatial and temporal trends in the location of the lifetime maximum intensity of tropical cyclones
publisher MDPI AG
publishDate 2017
url https://doi.org/10.3390/atmos8100198
https://doaj.org/article/d11c933b63a84e3486f77c51fc5be2ff
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere, Vol 8, Iss 10, p 198 (2017)
op_relation https://www.mdpi.com/2073-4433/8/10/198
https://doaj.org/toc/2073-4433
2073-4433
doi:10.3390/atmos8100198
https://doaj.org/article/d11c933b63a84e3486f77c51fc5be2ff
op_doi https://doi.org/10.3390/atmos8100198
container_title Atmosphere
container_volume 8
container_issue 12
container_start_page 198
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