机构地区:[1]National Meteorological Center,China Meteorological Administration,Beijing 100081 [2]Numerical Weather Prediction Center of China Meteorological Administration,Beijing 100081 [3]College of Global Change and Earth System Science,Beijing Normal University,Beijing 100875
出 处:《Journal of Meteorological Research》2019年第4期734-746,共13页气象学报(英文版)
基 金:Supported by the Youth Talent Development Program of China Meteorological Administration(201702);National Key Research and Development Program of China(2017YFC1501406 and 2017YFA0604502)
摘 要:This study used the Global/Regional Assimilation and PrEdiction System Single-Column Model(GRAPES_SCM)to simulate monsoon precipitation with deep convective cloud and associated cirrus during the Tropical Warm Pool International Cloud Experiment(TWP-ICE),especially during the active and suppressed monsoon periods.Four cases with different heterogeneous nucleation parameterizations were simulated by using the ensemble method.All simulations clearly separated the active and suppressed monsoon periods,and they reproduced the major characteristics of monsoonal cloud such as the total cloud hydrometeor mixing ratio distribution,and precipitation and radiation properties.The results showed that the number concentration production rate of different heterogeneous nucleation parameterizations varied substantially under the given temperature and water vapor mixing ratio.However,ice formation and precipitation during the monsoon period were affected only slightly by the different heterogeneous nucleation parameterizations.This study also captured clear competition between different ice formation processes.This study used the Global/Regional Assimilation and PrEdiction System Single-Column Model(GRAPES_SCM)to simulate monsoon precipitation with deep convective cloud and associated cirrus during the Tropical Warm Pool International Cloud Experiment(TWP-ICE), especially during the active and suppressed monsoon periods. Four cases with different heterogeneous nucleation parameterizations were simulated by using the ensemble method. All simulations clearly separated the active and suppressed monsoon periods, and they reproduced the major characteristics of monsoonal cloud such as the total cloud hydrometeor mixing ratio distribution,and precipitation and radiation properties. The results showed that the number concentration production rate of different heterogeneous nucleation parameterizations varied substantially under the given temperature and water vapor mixing ratio. However, ice formation and precipitation during the monsoon period were affected only slightly by the different heterogeneous nucleation parameterizations. This study also captured clear competition between different ice formation processes.
关 键 词:Liuma MICROPHYSICS scheme MONSOON precipitation cloud MICROPHYSICS heterogeneous NUCLEATION GRAPES_SCM
分 类 号:TG1[金属学及工艺—金属学]
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