Evaluation of RegCM4 in simulating the interannual and interdecadal variations of Meiyu rainfall in China

被引:9
|
作者
Hu, Yijia [1 ]
Zhong, Zhong [1 ,2 ]
Lu, Wei [1 ]
Zhang, Yaocun [2 ]
Sun, Yuan [1 ]
机构
[1] PLA Univ Sci & Technol, Coll Meteorol & Oceanog, Nanjing 211101, Jiangsu, Peoples R China
[2] Nanjing Univ, Sch Atmospher Sci, Nanjing 210008, Jiangsu, Peoples R China
基金
中国国家自然科学基金;
关键词
ASIAN SUMMER MONSOON; WATER-VAPOR TRANSPORT; EAST-ASIA; VARIABILITY; PRECIPITATION; BAIU; ASSOCIATION; CONVECTION; RESOLUTION; FEATURES;
D O I
10.1007/s00704-015-1459-1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this paper, the performance of the regional climate model (RegCM4) in simulating the interannual and interdecadal variation of Meiyu rainfall over lower and middle reaches of Yangtze River (LMRYR) in China is evaluated. The results show that the bias of the simulated Meiyu rainfall exhibits some uncertainties and obvious interdecadal variation similar with that of Meiyu rainfall itself. The rainfall bias and its interdecadal variation have little impact on the simulation of the interannual variation of the Meiyu rainfall. Not only the amplitude but also the phase of the interannual variation of the Meiyu rainfall can be reproduced by the RegCM4. However, the interdecadal variation of the rainfall bias has large impacts on the model's performance in simulating the interdecadal component of the Meiyu rainfall, leading to lower skill of RegCM4 in simulating the interdecadal variation of the Meiyu rainfall than that in simulating the interannual variation. In addition, the interannual signals of the temperature, humidity, and vorticity in the lower troposphere in the large-scale NCEP lateral boundary force are stronger than the interdecadal signals, and the model can respond well to these interannual signals. Therefore, the RegCM4 has better performance in simulating the interannual variation of water vapor budget than the interdecadal variation, which further favors the simulation of the Meiyu rainfall at interannual time scale.
引用
收藏
页码:757 / 767
页数:11
相关论文
共 50 条
  • [31] Interannual and interdecadal variations in heat content of the upper ocean of the South China Sea
    He Y.
    Guan C.
    Gan Z.
    Advances in Atmospheric Sciences, 1997, 14 (2) : 271 - 276
  • [32] Interdecadal change of external forcings of March rainfall interannual variation over southern China
    Xiao, Yanxi
    Qiao, Yunting
    Jian, Maoqiu
    CLIMATE DYNAMICS, 2023, 61 (1-2) : 729 - 744
  • [33] Causes of the interdecadal transition in interannual variability of summertime intraseasonal rainfall over Southern China
    Lu, Wei
    Zhu, Yimin
    Hu, Yijia
    Zhong, Zhong
    Ha, Yao
    FRONTIERS IN ENVIRONMENTAL SCIENCE, 2022, 10
  • [34] Linear relationship between the interdecadal and interannual variabilities of North China rainfall in rainy season
    Lu, RY
    CHINESE SCIENCE BULLETIN, 2003, 48 (10): : 1040 - 1044
  • [35] Linear relationship between the interdecadal and interannual variabilities of North China rainfall in rainy season
    LU Riyu Institute of Atmospheric Physics
    Chinese Science Bulletin, 2003, (10) : 1040 - 1044
  • [36] Interdecadal change of external forcings of March rainfall interannual variation over southern China
    Yanxi Xiao
    Yunting Qiao
    Maoqiu Jian
    Climate Dynamics, 2023, 61 : 729 - 744
  • [37] Understanding the contribution of the vegetation-runoff system for simulating the African climate using the RegCM4 model
    Samy A. Anwar
    Theoretical and Applied Climatology, 2019, 138 : 1219 - 1230
  • [38] Simulating the Potential Evapotranspiration of Egypt Using the RegCM4: Sensitivity to the Land Surface and Boundary Layer Parameterizations
    Anwar, Samy A.
    Olusegun, Christiana F.
    HYDROLOGY, 2024, 11 (08)
  • [39] SIMULATION OF TROPICAL CYCLONES OVER THE WESTERN NORTH PACIFIC AND LANDFALLING IN CHINA BY REGCM4
    吴婕
    高学杰
    JournalofTropicalMeteorology, 2019, 25 (04) : 437 - 447
  • [40] Regional rainstorm changes in China: Ensemble projection via RegCM4 dynamical downscaling
    Zhou B.
    Cai Y.
    Han Z.
    Earth Science Frontiers, 2022, 29 (05) : 410 - 419