Inter-Research > CR > v76 > n2 > p177-189  
CR
Climate Research

via Mailchimp

CR 76:177-189 (2018)  -  DOI: https://doi.org/10.3354/cr01533

Leading interannual variability modes of East Asian winter precipitation in CMIP5 general circulation models

Chenxi Jin1, Yang Yang2,*, Wenli Guo1

1Beijing Meteorological Service Center, Beijing 100089, PR China
2Institute of Urban Meteorology, China Meteorological Administration, Beijing 100089, PR China
*Corresponding author:

ABSTRACT: This study examined the performances of 19 atmospheric general circulation models, which participated in Coupled Model Intercomparison Project 5 (CMIP5), while simulating East Asian winter (JFM) precipitation. The first 3 leading interannual variability modes of East Asian winter precipitation were obtained using the empirical orthogonal function (EOF) method. Results indicated that the observed first EOF mode, which accounted for 59% of the total variance and is ENSO related, represented a positive precipitation center over southern China. Specifically, the warm sea surface temperature (SST) in the equatorial central eastern Pacific induces an anomalous Philippine Sea anticyclone, and the increased southwesterly winds further transport anomalous water vapor to southern China, which causes more precipitation. EOF1 was well reproduced in the multimodel ensemble mean (MME), with a pattern correlation coefficient (PCC) of 0.84 and a temporal correlation coefficient (TCC) of 0.61. The observed EOF2 exhibited a north-south seesaw pattern, which may be forced by both the western Indian Ocean SST and the high-latitude wave train. The MME partially captured its spatial pattern (with a PCC of 0.48); however, it failed to reproduce its temporal variation (with a TCC of 0.17). The observed EOF3 exhibited an east-west dipole pattern, which was an Arctic Oscillation (AO)-related mode. In the negative AO phase, the strengthened East Asian trough at 500 hPa and the anomalous northerlies were observed to suppress precipitation over East Asia. However, almost all the models, including the MME, poorly simulated the temporal variation of EOF3 because the AO was considered to be an internal mode of the atmosphere.


KEY WORDS: CMIP5 · Winter precipitation · Interannual · Leading modes · ENSO · AO


Full text in pdf format 
Cite this article as: Jin C, Yang Y, Guo W (2018) Leading interannual variability modes of East Asian winter precipitation in CMIP5 general circulation models. Clim Res 76:177-189. https://doi.org/10.3354/cr01533

Export citation
Mail this link - Contents Mailing Lists - RSS
Facebook - - linkedIn