A Historical Perspective of the La Niña Event in 2020/2021

Li, Xiaofan; Hu, Zeng‐Zhen; Tseng, Yu‐heng; Liu, Yunyun; Liang, Ping

doi:10.1029/2021jd035546

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A Historical Perspective of the La Niña Event in 2020/2021

2022
By Li, Xiaofan ; Hu, Zeng‐Zhen ; Tseng, Yu‐heng ; ...
Source: Journal of Geophysical Research: Atmospheres, 127(7)

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Journal Title:

Journal of Geophysical Research: Atmospheres
Personal Author:

Li, Xiaofan ; Hu, Zeng‐Zhen ; Tseng, Yu‐heng ; Liu, Yunyun ; Liang, Ping

Li, Xiaofan ; Hu, Zeng‐Zhen ; Tseng, Yu‐heng ; Liu, Yunyun ; Liang, Ping Less -
NOAA Program & Office:

NWS (National Weather Service) ; CPC (Climate Prediction Center) ; NCEP (National Centers for Environmental Prediction)

NWS (National Weather Service) ; CPC (Climate Prediction Center) ; NCEP (National Centers for Environmental Prediction) Less -
Description:

El Niño–Southern Oscillation is the strongest interannual variability in the tropical oceans and the major source of global climate predictability. In this work, we examine the evolution of oceanic and atmospheric anomalies in the tropical Pacific during 2020/2021 La Niña and compare it with the historical strong La Niña events since 1982, identify the contributions of different time scale components, and assess the predictions and the impact on extra-tropical climate. 2020/2021 La Niña emerged in August 2020 and dissipated in May 2021. 2020/2021 La Niña was uniquely preceded by a borderline El Niño instead of an El Niño and a weak equatorial-heat discharge process. That resulted in the weakest event among the strong La
Keywords:

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Atmospheric Science Earth And Planetary Sciences (miscellaneous) Geophysics Space And Planetary Science
Source:

Journal of Geophysical Research: Atmospheres, 127(7)
DOI:

https://doi.org/10.1029/2021jd035546
ISSN:

2169-897X;2169-8996;
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PDF
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American Geophysical Union (AGU)
Document Type:

Journal Article
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urn:sha256:6e86bbdcd24835d19a7201bc0da3e4de57cd4e16e0bd3219bf480ae34f258cef
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https://repository.library.noaa.gov/view/noaa/53889/noaa_53889_DS1.pdf
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