East Asian summer precipitation in AWI-CM3: Comparison with observations and CMIP6 models

被引:2
|
作者
Shi, Jian [1 ,2 ]
Stepanek, Christian [1 ]
Sein, Dmitry [1 ]
Streffing, Jan [1 ,3 ]
Lohmann, Gerrit [1 ,4 ]
机构
[1] Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, Bremerhaven, Germany
[2] Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteorol, Key Lab Meteorol Disaster, Minist Educ, Nanjing, Peoples R China
[3] Jacobs Univ Bremen, Bremen, Germany
[4] Univ Bremen, Bremen, Germany
基金
中国国家自然科学基金;
关键词
AWI-CM3; CMIP6; East Asia; summer precipitation; PACIFIC DOUBLE ITCZ; UPPER-OCEAN BIASES; CONVECTION PARAMETERIZATION; MONSOON PRECIPITATION; HORIZONTAL RESOLUTION; CHINA; SIMULATION; ROLES; SHIFT;
D O I
10.1002/joc.8075
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Owing to the complicated spatial-temporal characteristics of East Asian precipitation (EAP), climate models have limited skills in simulating the modern Asian climate. This consequently leads to large uncertainties in simulations of the past EAP variation and future projections. Here, we explore the performance of the newly developed Alfred Wegener Institute Climate Model, version 3 (AWI-CM3) in simulating the climatological summer EAP. To test whether the model's skill depends on its atmosphere resolution, we design two AWI-CM3 simulations with different horizontal resolutions. The result shows that both simulations have acceptable performance in simulating the summer mean EAP, generally better than the majority of individual models participating in the Coupled Model Intercomparison Project (CMIP6). However, for the monthly EAP from June to August, AWI-CM3 exhibits a decayed skill, which is due to the subseasonal movement of the western Pacific subtropical high bias. The higher-resolution AWI-CM3 simulation shows an overall improvement relative to the one performed at a relatively lower resolution in all aspects taken into account regarding the EAP. We conclude that AWI-CM3 is a suitable tool for exploring the EAP for the observational period. Having verified the model's skill for modern climate, we suggest employing the AWI-CM3, especially with high atmosphere resolution, both for applications in paleoclimate studies and future projections.
引用
收藏
页码:4083 / 4098
页数:16
相关论文
共 50 条
  • [1] Comparison of CMIP6 and CMIP5 simulations of precipitation in China and the East Asian summer monsoon
    Xin, Xiaoge
    Wu, Tongwen
    Zhang, Jie
    Yao, Junchen
    Fang, Yongjie
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2020, 40 (15) : 6423 - 6440
  • [2] Annual Cycle of East Asian Precipitation Simulated by CMIP6 Models
    Yan, Yuhan
    Zhu, Congwen
    Liu, Boqi
    Jiang, Song
    [J]. ATMOSPHERE, 2021, 12 (01) : 1 - 16
  • [3] Simulations for CMIP6 With the AWI Climate Model AWI-CM-1-1
    Semmler, Tido
    Danilov, Sergey
    Gierz, Paul
    Goessling, Helge F.
    Hegewald, Jan
    Hinrichs, Claudia
    Koldunov, Nikolay
    Khosravi, Narges
    Mu, Longjiang
    Rackow, Thomas
    Sein, Dmitry, V
    Sidorenko, Dmitry
    Wang, Qiang
    Jung, Thomas
    [J]. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2020, 12 (09)
  • [4] Future Changes in the Relationship Between the South and East Asian Summer Monsoons in CMIP6 Models
    Chen, Hong-Jing
    Song, Yang
    Wei, Wei
    [J]. JOURNAL OF TROPICAL METEOROLOGY, 2023, 29 (02) : 191 - 203
  • [5] Future Changes in the Relationship Between the South and East Asian Summer Monsoons in CMIP6 Models
    陈虹静
    杨崧
    魏维
    [J]. Journal of Tropical Meteorology, 2023, 29 (02) : 191 - 203
  • [6] Influence of the Interdecadal Pacific Oscillation on South Asian and East Asian summer monsoon rainfall in CMIP6 models
    Chinta, Veeranjaneyulu
    Chen, Zesheng
    Du, Yan
    Chowdary, Jasti S.
    [J]. CLIMATE DYNAMICS, 2022, 58 (5-6) : 1791 - 1809
  • [7] Influence of the Interdecadal Pacific Oscillation on South Asian and East Asian summer monsoon rainfall in CMIP6 models
    Veeranjaneyulu Chinta
    Zesheng Chen
    Yan Du
    Jasti S. Chowdary
    [J]. Climate Dynamics, 2022, 58 : 1791 - 1809
  • [8] South Asian summer rainfall from CMIP3 to CMIP6 models: biases and improvements
    Linqiang He
    Tianjun Zhou
    Xiaolong Chen
    [J]. Climate Dynamics, 2023, 61 : 1049 - 1061
  • [9] South Asian summer rainfall from CMIP3 to CMIP6 models: biases and improvements
    He, Linqiang
    Zhou, Tianjun
    Chen, Xiaolong
    [J]. CLIMATE DYNAMICS, 2023, 61 (3-4) : 1049 - 1061
  • [10] Diversity of the climatological seasonal march of East Asian summer monsoon rainfall among the CMIP6 models
    Yu, Tiantian
    Chen, Wen
    Gong, Hainan
    Lan, Xiaoqing
    Li, Chaofan
    [J]. Global and Planetary Change, 2024, 241