Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau

Most global circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 6 (CMIP6) simulate a delayed onset of the tropical Asian summer monsoon of 3–6 pentads when compared with the observations. However, a clear explanation of this model bias has yet to be developed. This study i...

Full description

Bibliographic Details
Main Authors: Die Hu, Anmin Duan, Yuheng Tang, Wei Yu
Format: Article
Language:English
Published: IOP Publishing 2023-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/acff79
_version_ 1797661253806587904
author Die Hu
Anmin Duan
Yuheng Tang
Wei Yu
author_facet Die Hu
Anmin Duan
Yuheng Tang
Wei Yu
author_sort Die Hu
collection DOAJ
description Most global circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 6 (CMIP6) simulate a delayed onset of the tropical Asian summer monsoon of 3–6 pentads when compared with the observations. However, a clear explanation of this model bias has yet to be developed. This study indicates that 23 of the 31 of CMIP6 models generate both the Tibetan Plateau (TP) cold bias and the delayed monsoon onset across tropical Asia. The aloft TP cold air temperature associated with these models tends to reduce the land–sea thermal contrast and monsoon circulation, and hence it generates a delayed onset for the tropical summer monsoon. Two sensitivity experiments based on a coupled ocean–atmosphere–land GCM, together with additional data analysis, further confirm the underlying connection between monsoon onset and temperature anomaly over the TP. Therefore, it is of great importance that we attempt to reduce the model bias associated with the simulation of monsoon onset by improving the physical process parameterization scheme related to the TP temperatures.
first_indexed 2024-03-11T18:42:44Z
format Article
id doaj.art-6c0c083431404fda83e2ac958c9dd803
institution Directory Open Access Journal
issn 1748-9326
language English
last_indexed 2024-03-11T18:42:44Z
publishDate 2023-01-01
publisher IOP Publishing
record_format Article
series Environmental Research Letters
spelling doaj.art-6c0c083431404fda83e2ac958c9dd8032023-10-12T10:26:41ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-01181111400510.1088/1748-9326/acff79Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan PlateauDie Hu0https://orcid.org/0000-0003-0482-7585Anmin Duan1https://orcid.org/0000-0002-3022-2582Yuheng Tang2https://orcid.org/0000-0002-9639-3958Wei Yu3State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; College of Earth Science, University of Chinese Academy of Sciences , Beijing, People’s Republic of ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; College of Earth Science, University of Chinese Academy of Sciences , Beijing, People’s Republic of China; Center for Marine Meteorology and Climate Change, State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University , Xiamen, People’s Republic of ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; College of Earth Science, University of Chinese Academy of Sciences , Beijing, People’s Republic of ChinaSouthern Marine Science and Engineering Guangdong Laboratory (Zhuhai), School of Atmospheric Sciences, Sun Yat-sen University , Zhuhai, People’s Republic of ChinaMost global circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 6 (CMIP6) simulate a delayed onset of the tropical Asian summer monsoon of 3–6 pentads when compared with the observations. However, a clear explanation of this model bias has yet to be developed. This study indicates that 23 of the 31 of CMIP6 models generate both the Tibetan Plateau (TP) cold bias and the delayed monsoon onset across tropical Asia. The aloft TP cold air temperature associated with these models tends to reduce the land–sea thermal contrast and monsoon circulation, and hence it generates a delayed onset for the tropical summer monsoon. Two sensitivity experiments based on a coupled ocean–atmosphere–land GCM, together with additional data analysis, further confirm the underlying connection between monsoon onset and temperature anomaly over the TP. Therefore, it is of great importance that we attempt to reduce the model bias associated with the simulation of monsoon onset by improving the physical process parameterization scheme related to the TP temperatures.https://doi.org/10.1088/1748-9326/acff79CMIP6Asian summer monsoon onsetTibetan Plateaucold bias
spellingShingle Die Hu
Anmin Duan
Yuheng Tang
Wei Yu
Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
Environmental Research Letters
CMIP6
Asian summer monsoon onset
Tibetan Plateau
cold bias
title Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
title_full Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
title_fullStr Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
title_full_unstemmed Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
title_short Delayed onset of the tropical Asian summer monsoon in CMIP6 can be linked to the cold bias over the Tibetan Plateau
title_sort delayed onset of the tropical asian summer monsoon in cmip6 can be linked to the cold bias over the tibetan plateau
topic CMIP6
Asian summer monsoon onset
Tibetan Plateau
cold bias
url https://doi.org/10.1088/1748-9326/acff79
work_keys_str_mv AT diehu delayedonsetofthetropicalasiansummermonsoonincmip6canbelinkedtothecoldbiasoverthetibetanplateau
AT anminduan delayedonsetofthetropicalasiansummermonsoonincmip6canbelinkedtothecoldbiasoverthetibetanplateau
AT yuhengtang delayedonsetofthetropicalasiansummermonsoonincmip6canbelinkedtothecoldbiasoverthetibetanplateau
AT weiyu delayedonsetofthetropicalasiansummermonsoonincmip6canbelinkedtothecoldbiasoverthetibetanplateau