The southward shift of hurricane genesis over the northern Atlantic Ocean

Abstract The hurricane, with maximum wind speed over 64 kts, is among the most terrible calamities over the northern Atlantic (NATL). Previous studies identified a poleward migration of tropical cyclone (TC) genesis over the Pacific Ocean, but the shift over the NATL is statistically insignificant....

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Main Authors: Xi Cao, Renguang Wu, Xianling Jiang, Yifeng Dai, Pengfei Wang, Lei Zhou, Liang Wu, Difei Deng, Ying Sun, Shangfeng Chen, Kaiming Hu, Zhibiao Wang, Lu Liu, Xiaoqing Lan, Zhencai Du, Junhu Zhao, Xiao Xiao
Format: Article
Language:English
Published: Nature Portfolio 2025-01-01
Series:npj Climate and Atmospheric Science
Online Access:https://doi.org/10.1038/s41612-025-00923-2
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author Xi Cao
Renguang Wu
Xianling Jiang
Yifeng Dai
Pengfei Wang
Lei Zhou
Liang Wu
Difei Deng
Ying Sun
Shangfeng Chen
Kaiming Hu
Zhibiao Wang
Lu Liu
Xiaoqing Lan
Zhencai Du
Junhu Zhao
Xiao Xiao
author_facet Xi Cao
Renguang Wu
Xianling Jiang
Yifeng Dai
Pengfei Wang
Lei Zhou
Liang Wu
Difei Deng
Ying Sun
Shangfeng Chen
Kaiming Hu
Zhibiao Wang
Lu Liu
Xiaoqing Lan
Zhencai Du
Junhu Zhao
Xiao Xiao
author_sort Xi Cao
collection DOAJ
description Abstract The hurricane, with maximum wind speed over 64 kts, is among the most terrible calamities over the northern Atlantic (NATL). Previous studies identified a poleward migration of tropical cyclone (TC) genesis over the Pacific Ocean, but the shift over the NATL is statistically insignificant. The present study detects a robust southward migration in the genesis latitude of NATL TCs that later reach hurricane strength after 1979, which is consistent with a growth in hurricane frequency in the southern part (10°-20°N) of NATL. This increasing trend of hurricane frequency is intimately attributable to the decreasing vertical shear of zonal wind, resulting from a decreasing north-south temperature gradient. The reduced north-south temperature gradient is primarily caused by greater warming trend in tropospheric temperature in the subtropics, driven by intensified static stability. The present research suggests a potential increase in the hazards confronted by low-latitude islands and coastal nations in Northern America.
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series npj Climate and Atmospheric Science
spelling doaj-art-1fb9985bdcec4275a73f5140226a7e822025-02-02T12:14:41ZengNature Portfolionpj Climate and Atmospheric Science2397-37222025-01-018111010.1038/s41612-025-00923-2The southward shift of hurricane genesis over the northern Atlantic OceanXi Cao0Renguang Wu1Xianling Jiang2Yifeng Dai3Pengfei Wang4Lei Zhou5Liang Wu6Difei Deng7Ying Sun8Shangfeng Chen9Kaiming Hu10Zhibiao Wang11Lu Liu12Xiaoqing Lan13Zhencai Du14Junhu Zhao15Xiao Xiao16Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesSchool of Earth Sciences, Zhejiang UniversityKey Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan ProvinceTongji Zhejiang CollegeCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesKey Laboratory of Polar Ecosystem and Climate Change, Shanghai Jiao Tong University, Ministry of EducationCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesUniversity of New South WalesNational Climate Center, China Meteorological AdministrationCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesState Key Laboratory of Severe Weather, Chinese Academy of Meteorological SciencesCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesCenter for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of SciencesNational Climate Center, China Meteorological AdministrationChengdu Meteorological BureauAbstract The hurricane, with maximum wind speed over 64 kts, is among the most terrible calamities over the northern Atlantic (NATL). Previous studies identified a poleward migration of tropical cyclone (TC) genesis over the Pacific Ocean, but the shift over the NATL is statistically insignificant. The present study detects a robust southward migration in the genesis latitude of NATL TCs that later reach hurricane strength after 1979, which is consistent with a growth in hurricane frequency in the southern part (10°-20°N) of NATL. This increasing trend of hurricane frequency is intimately attributable to the decreasing vertical shear of zonal wind, resulting from a decreasing north-south temperature gradient. The reduced north-south temperature gradient is primarily caused by greater warming trend in tropospheric temperature in the subtropics, driven by intensified static stability. The present research suggests a potential increase in the hazards confronted by low-latitude islands and coastal nations in Northern America.https://doi.org/10.1038/s41612-025-00923-2
spellingShingle Xi Cao
Renguang Wu
Xianling Jiang
Yifeng Dai
Pengfei Wang
Lei Zhou
Liang Wu
Difei Deng
Ying Sun
Shangfeng Chen
Kaiming Hu
Zhibiao Wang
Lu Liu
Xiaoqing Lan
Zhencai Du
Junhu Zhao
Xiao Xiao
The southward shift of hurricane genesis over the northern Atlantic Ocean
npj Climate and Atmospheric Science
title The southward shift of hurricane genesis over the northern Atlantic Ocean
title_full The southward shift of hurricane genesis over the northern Atlantic Ocean
title_fullStr The southward shift of hurricane genesis over the northern Atlantic Ocean
title_full_unstemmed The southward shift of hurricane genesis over the northern Atlantic Ocean
title_short The southward shift of hurricane genesis over the northern Atlantic Ocean
title_sort southward shift of hurricane genesis over the northern atlantic ocean
url https://doi.org/10.1038/s41612-025-00923-2
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