Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models

Abstract The Pacific Walker circulation (WC) is a major component of the global climate system. It connects the Pacific sea surface temperature (SST) variability to the climate variabilities from the other ocean basins to the mid- and high latitudes. Previous studies indicated that the ENSO-related...

Full description

Bibliographic Details
Main Authors: Xin-Yue Wang, Jiang Zhu, Chueh-Hsin Chang, Nathaniel C. Johnson, Hailong Liu, Yadi Li, Chentao Song, Meijiao Xin, Yi Zhou, Xichen Li
Format: Article
Language:English
Published: SpringerOpen 2021-04-01
Series:Geoscience Letters
Subjects:
Online Access:https://doi.org/10.1186/s40562-021-00186-8
_version_ 1818941911184965632
author Xin-Yue Wang
Jiang Zhu
Chueh-Hsin Chang
Nathaniel C. Johnson
Hailong Liu
Yadi Li
Chentao Song
Meijiao Xin
Yi Zhou
Xichen Li
author_facet Xin-Yue Wang
Jiang Zhu
Chueh-Hsin Chang
Nathaniel C. Johnson
Hailong Liu
Yadi Li
Chentao Song
Meijiao Xin
Yi Zhou
Xichen Li
author_sort Xin-Yue Wang
collection DOAJ
description Abstract The Pacific Walker circulation (WC) is a major component of the global climate system. It connects the Pacific sea surface temperature (SST) variability to the climate variabilities from the other ocean basins to the mid- and high latitudes. Previous studies indicated that the ENSO-related atmospheric feedback, in particular, the surface wind response is largely underestimated in AMIP and CMIP models. In this study, we further investigate the responses in the WC stream function and the sea level pressure (SLP) to the ENSO-related SST variability by comparing the responses in 45 AMIP and 63 CMIP models and six reanalysis datasets. We reveal a diversity in the performances of simulated SLP and WC between different models. While the SLP responses to the El Niño-related SST variability are well simulated in most of the atmospheric and coupled models, the WC stream function responses are largely underestimated in most of these models. The WC responses in the AMIP5/6 models capture ~ 75% of those in the reanalysis, whereas the CMIP5/6 models capture ~ 58% of the responses. Further analysis indicates that these underestimated circulation responses could be partially attributed to the biases in the precipitation scheme in both the atmospheric and coupled models, as well as the biases in the simulated ENSO-related SST patterns in the coupled models. One should pay special attention to these biases when studying the WC or the tropical atmosphere–ocean interactions using numerical models.
first_indexed 2024-12-20T07:03:03Z
format Article
id doaj.art-a6ba2fb71edc4253ab9d0ccf0dc8c9e9
institution Directory Open Access Journal
issn 2196-4092
language English
last_indexed 2024-12-20T07:03:03Z
publishDate 2021-04-01
publisher SpringerOpen
record_format Article
series Geoscience Letters
spelling doaj.art-a6ba2fb71edc4253ab9d0ccf0dc8c9e92022-12-21T19:49:09ZengSpringerOpenGeoscience Letters2196-40922021-04-018111310.1186/s40562-021-00186-8Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled modelsXin-Yue Wang0Jiang Zhu1Chueh-Hsin Chang2Nathaniel C. Johnson3Hailong Liu4Yadi Li5Chentao Song6Meijiao Xin7Yi Zhou8Xichen Li9Institute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesCenter for Climate Change Prediction Research, Ewha Womans UniversityAtmospheric Oceanic Sciences Program, Princeton UniversityInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesInstitute of Atmospheric Physics, Chinese Academy of SciencesAbstract The Pacific Walker circulation (WC) is a major component of the global climate system. It connects the Pacific sea surface temperature (SST) variability to the climate variabilities from the other ocean basins to the mid- and high latitudes. Previous studies indicated that the ENSO-related atmospheric feedback, in particular, the surface wind response is largely underestimated in AMIP and CMIP models. In this study, we further investigate the responses in the WC stream function and the sea level pressure (SLP) to the ENSO-related SST variability by comparing the responses in 45 AMIP and 63 CMIP models and six reanalysis datasets. We reveal a diversity in the performances of simulated SLP and WC between different models. While the SLP responses to the El Niño-related SST variability are well simulated in most of the atmospheric and coupled models, the WC stream function responses are largely underestimated in most of these models. The WC responses in the AMIP5/6 models capture ~ 75% of those in the reanalysis, whereas the CMIP5/6 models capture ~ 58% of the responses. Further analysis indicates that these underestimated circulation responses could be partially attributed to the biases in the precipitation scheme in both the atmospheric and coupled models, as well as the biases in the simulated ENSO-related SST patterns in the coupled models. One should pay special attention to these biases when studying the WC or the tropical atmosphere–ocean interactions using numerical models.https://doi.org/10.1186/s40562-021-00186-8Pacific Walker circulationENSOAMIP5/6 and CMIP5/6 modelsAtmosphere–ocean interactionModel bias
spellingShingle Xin-Yue Wang
Jiang Zhu
Chueh-Hsin Chang
Nathaniel C. Johnson
Hailong Liu
Yadi Li
Chentao Song
Meijiao Xin
Yi Zhou
Xichen Li
Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
Geoscience Letters
Pacific Walker circulation
ENSO
AMIP5/6 and CMIP5/6 models
Atmosphere–ocean interaction
Model bias
title Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
title_full Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
title_fullStr Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
title_full_unstemmed Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
title_short Underestimated responses of Walker circulation to ENSO-related SST anomaly in atmospheric and coupled models
title_sort underestimated responses of walker circulation to enso related sst anomaly in atmospheric and coupled models
topic Pacific Walker circulation
ENSO
AMIP5/6 and CMIP5/6 models
Atmosphere–ocean interaction
Model bias
url https://doi.org/10.1186/s40562-021-00186-8
work_keys_str_mv AT xinyuewang underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT jiangzhu underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT chuehhsinchang underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT nathanielcjohnson underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT hailongliu underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT yadili underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT chentaosong underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT meijiaoxin underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT yizhou underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels
AT xichenli underestimatedresponsesofwalkercirculationtoensorelatedsstanomalyinatmosphericandcoupledmodels