Tropical cyclones act to intensify El Niño
While it is known that the El Niño–Southern Oscillation (ENSO) influences tropical cyclones, but little is known about a reverse effect. Here, data and model output shows that tropical cyclones can affect ENSO with a lead of 3 months, especially contributing to a significantly more intense El Niño i...
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2019-08-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-019-11720-w |
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doaj-023908e8ec834a678af9a2b8af039f8f2021-05-11T12:13:49ZengNature Publishing GroupNature Communications2041-17232019-08-0110111310.1038/s41467-019-11720-wTropical cyclones act to intensify El NiñoQiuyun Wang0Jianping Li1Fei-Fei Jin2Johnny C. L. Chan3Chunzai Wang4Ruiqiang Ding5Cheng Sun6Fei Zheng7Juan Feng8Fei Xie9Yanjie Li10Fei Li11Yidan Xu12College of Global Change and Earth System Sciences (GCESS), Beijing Normal UniversityKey Laboratory of Physical Oceanography/Institute for Advanced Ocean Studies, Ocean University of China and Qingdao National Laboratory for Marine Science and TechnologyDepartment of Atmospheric Sciences, University of Hawai’i at MānoaSchool of Energy and Environment, City University of Hong KongState Key Laboratory of Tropical Oceanography (LTO), South China Sea Institute of Oceanology, Chinese Academy of SciencesState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of SciencesCollege of Global Change and Earth System Sciences (GCESS), Beijing Normal UniversityState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of SciencesCollege of Global Change and Earth System Sciences (GCESS), Beijing Normal UniversityCollege of Global Change and Earth System Sciences (GCESS), Beijing Normal UniversityState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of SciencesDepartment of Lower Atmosphere Observation Research (LAOR), Institute of Atmospheric Physics, Chinese Academy of SciencesCollege of Global Change and Earth System Sciences (GCESS), Beijing Normal UniversityWhile it is known that the El Niño–Southern Oscillation (ENSO) influences tropical cyclones, but little is known about a reverse effect. Here, data and model output shows that tropical cyclones can affect ENSO with a lead of 3 months, especially contributing to a significantly more intense El Niño in the winter months.https://doi.org/10.1038/s41467-019-11720-w |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Qiuyun Wang Jianping Li Fei-Fei Jin Johnny C. L. Chan Chunzai Wang Ruiqiang Ding Cheng Sun Fei Zheng Juan Feng Fei Xie Yanjie Li Fei Li Yidan Xu |
spellingShingle |
Qiuyun Wang Jianping Li Fei-Fei Jin Johnny C. L. Chan Chunzai Wang Ruiqiang Ding Cheng Sun Fei Zheng Juan Feng Fei Xie Yanjie Li Fei Li Yidan Xu Tropical cyclones act to intensify El Niño Nature Communications |
author_facet |
Qiuyun Wang Jianping Li Fei-Fei Jin Johnny C. L. Chan Chunzai Wang Ruiqiang Ding Cheng Sun Fei Zheng Juan Feng Fei Xie Yanjie Li Fei Li Yidan Xu |
author_sort |
Qiuyun Wang |
title |
Tropical cyclones act to intensify El Niño |
title_short |
Tropical cyclones act to intensify El Niño |
title_full |
Tropical cyclones act to intensify El Niño |
title_fullStr |
Tropical cyclones act to intensify El Niño |
title_full_unstemmed |
Tropical cyclones act to intensify El Niño |
title_sort |
tropical cyclones act to intensify el niño |
publisher |
Nature Publishing Group |
series |
Nature Communications |
issn |
2041-1723 |
publishDate |
2019-08-01 |
description |
While it is known that the El Niño–Southern Oscillation (ENSO) influences tropical cyclones, but little is known about a reverse effect. Here, data and model output shows that tropical cyclones can affect ENSO with a lead of 3 months, especially contributing to a significantly more intense El Niño in the winter months. |
url |
https://doi.org/10.1038/s41467-019-11720-w |
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