Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America

Tropical Cyclones (TCs) and Easterly Waves (EWs) are the most important phenomena in Tropical North America. Thus, examining their future changes is crucial for adaptation and mitigation strategies. The Community Earth System Model drove a three-member regional model multi-physics ensemble under the...

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Published in:Oceans
Main Authors: Christian Dominguez, James M. Done, Cindy L. Bruyère
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/oceans2020024
https://doaj.org/article/b01d5bab17774dc2b8bae6af91acee0f
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spelling ftdoajarticles:oai:doaj.org/article:b01d5bab17774dc2b8bae6af91acee0f 2023-05-15T17:34:09+02:00 Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America Christian Dominguez James M. Done Cindy L. Bruyère 2021-06-01T00:00:00Z https://doi.org/10.3390/oceans2020024 https://doaj.org/article/b01d5bab17774dc2b8bae6af91acee0f EN eng MDPI AG https://www.mdpi.com/2673-1924/2/2/24 https://doaj.org/toc/2673-1924 doi:10.3390/oceans2020024 2673-1924 https://doaj.org/article/b01d5bab17774dc2b8bae6af91acee0f Oceans, Vol 2, Iss 24, Pp 429-447 (2021) tropical cyclones easterly waves future changes in rainfall changes in tropical cyclogenesis Oceanography GC1-1581 article 2021 ftdoajarticles https://doi.org/10.3390/oceans2020024 2022-12-31T10:25:56Z Tropical Cyclones (TCs) and Easterly Waves (EWs) are the most important phenomena in Tropical North America. Thus, examining their future changes is crucial for adaptation and mitigation strategies. The Community Earth System Model drove a three-member regional model multi-physics ensemble under the Representative Concentration Pathways 8.5 emission scenario for creating four future scenarios (2020–2030, 2030–2040, 2050–2060, 2080–2090). These future climate runs were analyzed to determine changes in EW and TC features: rainfall, track density, contribution to seasonal rainfall, and tropical cyclogenesis. Our study reveals that a mean increase of at least 40% in the mean annual TC precipitation is projected over northern Mexico and southwestern USA. Slight positive changes in EW track density are projected southwards 10° N over the North Atlantic Ocean for the 2050–2060 and 2080–2090 periods. Over the Eastern Pacific Ocean, a mean increment in the EW activity is projected westwards across the future decades. Furthermore, a mean reduction by up to 60% of EW rainfall, mainly over the Caribbean region, Gulf of Mexico, and central-southern Mexico, is projected for the future decades. Tropical cyclogenesis over both basins slightly changes in future scenarios (not significant). We concluded that these variations could have significant impacts on regional precipitation. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Oceans 2 2 429 447
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
Oceanography
GC1-1581
spellingShingle tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
Oceanography
GC1-1581
Christian Dominguez
James M. Done
Cindy L. Bruyère
Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
topic_facet tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
Oceanography
GC1-1581
description Tropical Cyclones (TCs) and Easterly Waves (EWs) are the most important phenomena in Tropical North America. Thus, examining their future changes is crucial for adaptation and mitigation strategies. The Community Earth System Model drove a three-member regional model multi-physics ensemble under the Representative Concentration Pathways 8.5 emission scenario for creating four future scenarios (2020–2030, 2030–2040, 2050–2060, 2080–2090). These future climate runs were analyzed to determine changes in EW and TC features: rainfall, track density, contribution to seasonal rainfall, and tropical cyclogenesis. Our study reveals that a mean increase of at least 40% in the mean annual TC precipitation is projected over northern Mexico and southwestern USA. Slight positive changes in EW track density are projected southwards 10° N over the North Atlantic Ocean for the 2050–2060 and 2080–2090 periods. Over the Eastern Pacific Ocean, a mean increment in the EW activity is projected westwards across the future decades. Furthermore, a mean reduction by up to 60% of EW rainfall, mainly over the Caribbean region, Gulf of Mexico, and central-southern Mexico, is projected for the future decades. Tropical cyclogenesis over both basins slightly changes in future scenarios (not significant). We concluded that these variations could have significant impacts on regional precipitation.
format Article in Journal/Newspaper
author Christian Dominguez
James M. Done
Cindy L. Bruyère
author_facet Christian Dominguez
James M. Done
Cindy L. Bruyère
author_sort Christian Dominguez
title Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title_short Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title_full Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title_fullStr Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title_full_unstemmed Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title_sort future changes in tropical cyclone and easterly wave characteristics over tropical north america
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/oceans2020024
https://doaj.org/article/b01d5bab17774dc2b8bae6af91acee0f
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Oceans, Vol 2, Iss 24, Pp 429-447 (2021)
op_relation https://www.mdpi.com/2673-1924/2/2/24
https://doaj.org/toc/2673-1924
doi:10.3390/oceans2020024
2673-1924
https://doaj.org/article/b01d5bab17774dc2b8bae6af91acee0f
op_doi https://doi.org/10.3390/oceans2020024
container_title Oceans
container_volume 2
container_issue 2
container_start_page 429
op_container_end_page 447
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