Impact of physical representations in CALMET on the simulated wind field over land during Super Typhoon Meranti(2016)  

作　　者：Sui HUANG Shengming TANG Hui YU Wenbo XUE Pingzhi FANG Peiyan CHEN 

机构地区：[1]Chinese Academy of Meteorological Sciences,Beijing 100081,China [2]Shanghai Typhoon Institute,China Meteorological Administration,Shanghai 200030,China [3]Key Laboratory of Numerical Modeling for Tropical Cyclones China Meteorological Administration,Shanghai 200030,China [4]The Joint Laboratory for Typhoon Forecasting Technique Applications between Shanghai Typhoon Institute and Wenzhou Meteorological Bureau,Wenzhou 325000,China

出　　处：《Frontiers of Earth Science》2019年第4期744-757,共14页地球科学前沿（英文版）

基　　金：This research was supported by the National Basic Research Program of China(No.2015CB452806);the National Natural Science Foundation of China(Nos.41805088,41875080);Natural Science Foundation of Shanghai(No.18ZR1449100);Fundamental Research Foundation of Shanghai Typhoon Institute of the China Meteorological Administration(Nos.2018JB05,2019JB06).

摘　　要：A WRF(Weather Research and Forecasting Model)/CALMET(California Meteorological Model)coupled system is used to investigate the impact of physical representations in CALMET on simulations of the near-surface wind field of Super Typhoon Meranti(2016).The coupled system is configured with a horizontal grid spacing of 3 km in WRF and 500 m in CALMET,respectively.The model performance of the coupled WRF/CALMET system is evaluated by comparing the results of simulations with observational data from 981 automatic surface stations in Fujian Province.The root mean square error(RMSE)of the wind speed at 10 m in all CALMET simulations is significantly less than the WRF simulation by 20%^30%,suggesting that the coupled WRF/CALMET system is capable of representing more realistic simulated wind speed than the mesoscale model only.The impacts of three physical representations including blocking effects,kinematic effects of terrain and slope flows in CALMET are examined in a specified local region called Shishe Mountain.The results show that before the typhoon landfall in Xiamen,a net downslope flow that is tangent to the terrain is generated in the west of Shishe Mountain due to blocking effects with magnitude exceeding 10 m/s.However,the blocking effects seem to take no effect in the strong wind area after typhoon landfall.Whether being affected by the typhoon strong wind or not,the slope flows move downslope at night and upslope in the daytime due to the diurnal variability of the local heat flux with magnitude smaller than 3 m/s.The kinematic effects of terrain,which are speculated to play a significant role in the typhoon strong wind area,can only be applied to atmospheric flows in stable conditions when the wind field is quasinondivergent.

关 键 词：physical representations CALMET wind field Super Typhoon Meranti 

分 类 号：P44[天文地球—大气科学及气象学]