Idealized simulations of tropical cyclones with thermodynamic conditions under reanalysis and CMIP5 scenarios

被引:0
|
作者
Cheng-Hsiang Chih
Kun-Hsuan Chou
Chun-Chieh Wu
机构
[1] National Taiwan University,Department of Atmospheric Sciences
[2] Chinese Culture University,Department of Atmospheric Sciences
[3] Academia Sinica,Research Center for Environmental Changes
来源
关键词
Tropical cyclone size; Climate change; Downscaling; Idealized simulation; Thermodynamic conditions;
D O I
暂无
中图分类号
学科分类号
摘要
The idealized Weather Research and Forecasting (WRF) simulations are conducted to investigate tropical cyclone (TC) size and intensity over the Western North Pacific (WNP) over the past decades, as represented by National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) R-1, European Center for Medium range Weather Forecasting (ECMWF) twentieth century (ERA20C) reanalysis, and National Oceanic and Atmospheric Administration Cooperative Institute for Research in Environmental Sciences 20th Century (CIRES20) Reanalysis V2 data, and under a future climate, as predicted by the Coupled Model Intercomparison Project Phase 5 (CMIP5). Firstly, sensitivity experiments with varying environmental thermodynamic forcing are conducted to examine how thermodynamic conditions affect TC size and intensity. Secondly, distributions of thermodynamic quantities taken from the NCEP/NCAR R-1, ERA20C, CIRES20, and CMIP5 data are used to initialize four more sets of WRF simulations. There is no significant variation in TC size nor intensity over the WNP within the past 90 years based on the idealized downscaling high-resolution WRF model, whereas those simulations initialized based on CMIP5 data show that both the TC size and intensity would increase in the future (2071–2100) of the representative concentration pathway 8.5 (RCP8.5) as compared to those during the current (2010–2040) climate stage of RCP8.5. An explanation for these findings is given by referring to impact of the air–sea thermal disequilibrium and acutely increasing temperature in the TC outflow, while their relation to previous works is also discussed.
引用
收藏
相关论文
共 50 条
  • [41] The Ability of CMIP5 Models to Simulate North Atlantic Extratropical Cyclones
    Zappa, Giuseppe
    Shaffrey, Len C.
    Hodges, Kevin I.
    JOURNAL OF CLIMATE, 2013, 26 (15) : 5379 - 5396
  • [42] The Tibetan Plateau Summer Monsoon in the CMIP5 Simulations
    Duan, Anmin
    Hu, Jun
    Xiao, Zhixiang
    JOURNAL OF CLIMATE, 2013, 26 (19) : 7747 - 7766
  • [43] The hiatus and accelerated warming decades in CMIP5 simulations
    Yi Song
    Yongqiang Yu
    Pengfei Lin
    Advances in Atmospheric Sciences, 2014, 31 : 1316 - 1330
  • [44] Intercomparison of the Surface Energy Partitioning in CMIP5 Simulations
    Yang, Jiachuan
    Wang, Zhi-Hua
    Huang, Huei-Ping
    ATMOSPHERE, 2019, 10 (10)
  • [45] Decadal Prediction of the Sahelian Precipitation in CMIP5 Simulations
    Gaetani, Marco
    Mohino, Elsa
    JOURNAL OF CLIMATE, 2013, 26 (19) : 7708 - 7719
  • [46] The hiatus and accelerated warming decades in CMIP5 simulations
    Song Yi
    Yu Yongqiang
    Lin Pengfei
    ADVANCES IN ATMOSPHERIC SCIENCES, 2014, 31 (06) : 1316 - 1330
  • [47] Anthropogenic forcing on the Hadley circulation in CMIP5 simulations
    Lijun Tao
    Yongyun Hu
    Jiping Liu
    Climate Dynamics, 2016, 46 : 3337 - 3350
  • [48] Anthropogenic forcing on the Hadley circulation in CMIP5 simulations
    Tao, Lijun
    Hu, Yongyun
    Liu, Jiping
    CLIMATE DYNAMICS, 2016, 46 (9-10) : 3337 - 3350
  • [49] Poleward expansion of the hadley circulation in CMIP5 simulations
    Yongyun Hu
    Lijun Tao
    Jiping Liu
    Advances in Atmospheric Sciences, 2013, 30 : 790 - 795
  • [50] Poleward Expansion of the Hadley Circulation in CMIP5 Simulations
    胡永云
    陶利军
    刘骥平
    Advances in Atmospheric Sciences, 2013, 30 (03) : 790 - 795