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: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/oceans2020024
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author Christian Dominguez
James M. Done
Cindy L. Bruyère
author_facet Christian Dominguez
James M. Done
Cindy L. Bruyère
author_sort Christian Dominguez
collection MDPI Open Access Publishing
container_issue 2
container_start_page 429
container_title Oceans
container_volume 2
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.
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spelling ftmdpi:oai:mdpi.com:/2673-1924/2/2/24/ 2025-01-16T23:41:37+00:00 Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America Christian Dominguez James M. Done Cindy L. Bruyère agris 2021-06-10 application/pdf https://doi.org/10.3390/oceans2020024 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/oceans2020024 https://creativecommons.org/licenses/by/4.0/ Oceans; Volume 2; Issue 2; Pages: 429-447 tropical cyclones easterly waves future changes in rainfall changes in tropical cyclogenesis Text 2021 ftmdpi https://doi.org/10.3390/oceans2020024 2023-08-01T01:55:42Z 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. Text North Atlantic MDPI Open Access Publishing Pacific Oceans 2 2 429 447
spellingShingle tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
Christian Dominguez
James M. Done
Cindy L. Bruyère
Future Changes in Tropical Cyclone and Easterly Wave Characteristics over Tropical North America
title 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_short 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
topic tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
topic_facet tropical cyclones
easterly waves
future changes in rainfall
changes in tropical cyclogenesis
url https://doi.org/10.3390/oceans2020024