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海洋飞沫方案改进对台风“威马逊”强度预报的影响
引用本文:段自强,李永平,于润玲,黄伟,郑运霞.海洋飞沫方案改进对台风“威马逊”强度预报的影响[J].海洋与湖沼,2016,47(6):1075-1090.
作者姓名:段自强  李永平  于润玲  黄伟  郑运霞
作者单位:中国气象局上海台风研究所 上海 200030,中国气象局上海台风研究所 上海 200030,中国气象局上海台风研究所 上海 200030,中国气象局上海台风研究所 上海 200030,中国气象局上海台风研究所 上海 200030
基金项目:国家重点基础研究发展计划(973)项目,2013CB430305号;“全球变化与海气相互作用”专项项目,GASI-IPOVAI-04号;中国气象局上海台风研究所基本科研业务专项项目,2016JB12号;上海市气象局科技开发项目,YJ201603号。
摘    要:本文采用分粒径段组合方式改进海气耦合模式海洋飞沫方案,并利用耦合模式对1409号台风"威马逊"进行数值模拟,分析了海洋飞沫方案改进对台风结构、强度以及海气动量通量、热量通量模拟结果的影响。结果显示,耦合模式中海洋飞沫方案可通过改变海表面粗糙度影响海气动量与热量通量;海洋飞沫还可以通过沫滴向大气输送感热和水汽而直接影响海气热通量,进一步影响台风的强度。模拟结果显示改进后海洋飞沫方案的台风强度更接近观测。改进海洋飞沫方案后粗糙度的计算结果小于原始方案,相应地海气热通量以及下垫面耗散作用也弱于后者,海表面风场是海气热交换与下垫面耗散共同作用的结果。

关 键 词:热带气旋  海洋飞沫  海气耦合  海气通量  台风强度
收稿时间:2/2/2016 12:00:00 AM
修稿时间:2016/6/25 0:00:00

ON TROPICAL CYCLONE INTENSITY FORECAST USING IMPROVED SEA SPRAY SCHEME IN REGIONAL ATMOSPHERE-WAVE COUPLED MODEL
DUAN Zi-Qiang,LI Yong-Ping,YU Run-Ling,HUANG Wei and ZHENG Yun-Xia.ON TROPICAL CYCLONE INTENSITY FORECAST USING IMPROVED SEA SPRAY SCHEME IN REGIONAL ATMOSPHERE-WAVE COUPLED MODEL[J].Oceanologia Et Limnologia Sinica,2016,47(6):1075-1090.
Authors:DUAN Zi-Qiang  LI Yong-Ping  YU Run-Ling  HUANG Wei and ZHENG Yun-Xia
Institution:Shanghai Typhoon Institute, CMA, Shanghai 200030, China,Shanghai Typhoon Institute, CMA, Shanghai 200030, China,Shanghai Typhoon Institute, CMA, Shanghai 200030, China,Shanghai Typhoon Institute, CMA, Shanghai 200030, China and Shanghai Typhoon Institute, CMA, Shanghai 200030, China
Abstract:A sea-spray parameterization scheme in tropical cyclone (TC) model was improved and it well performed at selected diameter domains.The super Typhoon Rammasun in 2014 was simulated to analyze the impact of the improved scheme on TC development.The TC structure,intensity,momentum flux,sensible heat flux,and latent heat flux were analyzed.The simulation result in the improved sea spray scheme was closer to the TC track.In the sea spray scheme,air-sea momentum and heat exchanges varied by changing sea surface roughness and droplet evaporation,the TC intensity and structure in the simulation were also changed,and the roughness was smaller than that in the original scheme.In addition,the sea surface wind was enhanced as the friction was weakened.On the other hand,the reduced roughness resulted in smaller sensible and latent heat fluxes and less energy supply for TC.The sea surface wind speed was controlled by the balance between friction mechanism and heat strengthening mechanism.
Keywords:tropical cyclone  sea spray  coupled atmosphere-wave model  air-sea flux  TC intensity
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