High resolution regional climate simulation over CORDEX East Asia phase II domain using the COAWST Ocean-atmosphere coupled model

被引:0
|
作者
Long, Mengyuan [1 ,2 ]
Yu, Ke [2 ,3 ]
Lu, Yutong [1 ,2 ,4 ]
Wang, Shuyu [2 ]
Tang, Jianping [1 ,2 ]
机构
[1] Nanjing Univ, Key Lab Mesoscale Severe Weather, Minist Educ, Nanjing, Peoples R China
[2] Nanjing Univ, Sch Atmospher Sci, 163 Xianlin Rd, Nanjing, Peoples R China
[3] PowerChina Huadong Engn Corp Ltd, Hangzhou, Peoples R China
[4] Univ Leeds, Inst Climate & Atmospher Sci, Sch Earth & Environm, Leeds, England
关键词
COAWST regional model; Ocean-atmosphere coupling; CORDEX East Asia; Surface air temperature; Summer precipitation; Boreal summer intra-seasonal oscillation; WESTERN NORTH PACIFIC; SUMMER MONSOON; INTERANNUAL VARIABILITY; SYSTEM; PROPAGATION; PARAMETERIZATION; EXPLICIT; SURFACE; SST;
D O I
10.1007/s00382-024-07356-2
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study reveals the simulation results of a regional ocean-atmosphere coupled model (Coupled Ocean-Atmosphere-Wave Sediment Transport Modeling System, COAWST) for the Coordinated Regional Climate Downscaling Experiment (CORDEX) East Asia Phase II, which covers a period of 21 years (1989-2009) at a horizontal resolution of 25 km. The coupled simulation (CPL) and the uncoupled atmospheric simulation (UNCPL) are compared with observations to assess their capability of capturing the climatology characteristics over East Asia. The simulated sea surface temperature (SST) in CPL is generally overestimated (underestimated) in summer (winter) over most CORDEX-EA-II regions. Both CPL and UNCPL can capture the spatial patterns of seasonal air temperature over East Asia well. However, they both simulate cold biases of the winter temperature over most regions of China. CPL can reduce the cold biases over certain regions, which may be related to the increased cloud cover reflecting more longwave radiation to the ground. Additionally, CPL improves the simulation results of summer precipitation, diminishing the dry biases over northern Bay of Bengal and South China Sea. This improvement may be related to the better description of moisture transportation and precipitable water. Furthermore, The CPL experiment can better simulate the inter-annual variability of summer precipitation and the relationship between SST and precipitation, especially over the South China Sea and Philippines Sea. CPL also captures the northward propagation and amplitude of boreal summer intra-seasonal oscillation precipitation anomalies more accurately. These findings highlight the importance of ocean-atmosphere coupling processes to simulate multiscale climate changes in the CORDEX-EA-II regions. center dot The COAWST regional coupled model enhances the simulation of surface air temperature and precipitation climatology over CORDEX East Asia.center dot The coupled model effectively represents the inter-annual variability of summer precipitation over most western Northern Pacific regions.center dot The coupled model provides a more accurate depiction of the northward propagation and amplitude of BSISO precipitation anomalies.
引用
收藏
页码:8711 / 8727
页数:17
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