How well do climate models simulate regional atmospheric circulation over East Asia?

被引:18
作者
Zhao, Can [1 ,2 ]
Jiang, Zhihong [2 ,3 ]
Sun, Xiaojuan [1 ,2 ]
Li, Wei [1 ,2 ]
Li, Laurent [4 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Joint Int Res Lab Climate & Environm Change, Nanjing, Peoples R China
[2] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ, Nanjing, Peoples R China
[4] Sorbonne Univ, Lab Meteorol Dynam, Ecole Polytech, Ecole Normale Super,CNRS, Paris, France
基金
中国国家自然科学基金;
关键词
atmospheric circulation; closed-circulation systems; CMIP5; models; Indian low; monsoon precipitation; South Asian high; western North Pacific subtropical high; NORTH-AMERICAN CLIMATE; WATER-VAPOR TRANSPORT; YANGTZE-RIVER VALLEY; INTERANNUAL VARIABILITY; SUMMER MONSOON; HISTORICAL SIMULATIONS; CMIP5; CHINA; PRECIPITATION; RAINFALL;
D O I
10.1002/joc.6205
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study presents a comprehensive and quantitative evaluation of the mean state of summer atmospheric circulation over East Asia. Attention is paid to the South Asian high (SAH), western North Pacific subtropical high (WNPSH) and Indian low (IL) at the upper, middle and lower troposphere, respectively. A total of 31 state-of-the-art climate models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) are used as examples for the analysis. Most models can basically simulate the three closed-circulation systems (CCSs), although there is a certain inter-model spread and an underestimation of their intensity. In terms of geographic location, models demonstrated the best performance for SAH and the poorest performance for WNPSH. The latter shows a generally south-westward shift compared to the National Centers for Environmental Prediction (NCEP) reanalysis. Five atmospheric fields (zonal and meridional wind at 850 hPa, geopotential height at 500 and 100 hPa and sea level pressure) are inspected and generally well reproduced in models, with Taylor-S indices all larger than 0.84 for 90% of the models. The best performance is for the geopotential height of 500 hPa with an average Taylor-S index of 0.98. Models' skill in simulating the sea level pressure is the lowest. However, a significant positive correlation with models' resolution is observed. Almost all models underestimate the 100 hPa geopotential height over East Asia, mainly due to the common cold bias in the troposphere. As a whole, CCSM4, CNRM-CM5, CESM1-CAM5 and NorESM1-M are identified as high-skill models for simulating the East Asian atmospheric circulation. High-skill models also show better simulation of precipitations in East China, with a 21.3% decrease of dry biases in Southeast China. The physical explanation for this linkage is also reported to reside in the central position of the WNPSH, which determines the quality of 850 hPa winds and water vapour transport in Southeast China.
引用
收藏
页码:220 / 234
页数:15
相关论文
共 62 条
  • [1] Akiyama T., 1975, Journal of the Meteorological Society of Japanese Series II, V53, P304, DOI [10.2151/jmsj1965.53.5_304, DOI 10.2151/JMSJ1965.53.5_304]
  • [2] Current and future atmospheric circulation at 500 hPa over Greenland simulated by the CMIP3 and CMIP5 global models
    Belleflamme, Alexandre
    Fettweis, Xavier
    Lang, Charlotte
    Erpicum, Michel
    [J]. CLIMATE DYNAMICS, 2013, 41 (7-8) : 2061 - 2080
  • [3] Spatial Interpolation of Daily Precipitation in China: 1951-2005
    Chen, Deliang
    Ou, Tinghai
    Gong, Lebing
    Xu, Chong-Yu
    Li Weijing
    Ho, Chang-Hoi
    Qian Weihong
    [J]. ADVANCES IN ATMOSPHERIC SCIENCES, 2010, 27 (06) : 1221 - 1232
  • [4] A comprehensive evaluation of precipitation simulations over China based on CMIP5 multimodel ensemble projections
    Chen, Liang
    Frauenfeld, Oliver W.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2014, 119 (10) : 5767 - 5786
  • [5] Probabilistic Projections of Climate Change over China under the SRES A1B Scenario Using 28 AOGCMs
    Chen, Weilin
    Jiang, Zhihong
    Li, Laurent
    [J]. JOURNAL OF CLIMATE, 2011, 24 (17) : 4741 - 4756
  • [6] The Tibetan Plateau Summer Monsoon in the CMIP5 Simulations
    Duan, Anmin
    Hu, Jun
    Xiao, Zhixiang
    [J]. JOURNAL OF CLIMATE, 2013, 26 (19) : 7747 - 7766
  • [7] Spatial variability of the Caribbean mid-summer drought and relation to north Atlantic high circulation
    Gamble, Douglas W.
    Parnell, Darren B.
    Curtis, Scott
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2008, 28 (03) : 343 - 350
  • [8] Performance metrics for climate models
    Gleckler, P. J.
    Taylor, K. E.
    Doutriaux, C.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D6)
  • [9] The Climatology and Interannual Variability of the East Asian Winter Monsoon in CMIP5 Models
    Gong, Hainan
    Wang, Lin
    Chen, Wen
    Wu, Renguang
    Wei, Ke
    Cui, Xuefeng
    [J]. JOURNAL OF CLIMATE, 2014, 27 (04) : 1659 - 1678
  • [10] Relationship of Sahel Precipitation and Atmospheric Centers of Action
    Hameed, Sultan
    Riemer, Nicole
    [J]. ADVANCES IN METEOROLOGY, 2012, 2012