云滴谱湍流拓宽和暖雨形成过程:综述(英文)
Broadening of cloud droplet size distributions and warm rain initiation associated with turbulence: an overview作者机构:Key Laboratory of Meteorological Disaster Ministry of Education(KLME)/Joint International Research Laboratory of Climate and Environment Change(ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters(CIC-FEMD)/Key Laboratory for Aerosol–Cloud–Precipitation of China Meteorological Administration Nanjing University of Information Science & Technology Ministry of Education Key Laboratory for Earth System Modeling and Department for Earth System Science Tsinghua University Environmental and Climate Sciences Department Brookhaven National Laboratory
出 版 物:《Atmospheric and Oceanic Science Letters》 (大气和海洋科学快报(英文版))
年 卷 期:2018年第11卷第2期
页 面:123-135页
核心收录:
学科分类:0710[理学-生物学] 0908[农学-水产] 07[理学] 0707[理学-海洋科学] 070601[理学-气象学] 0706[理学-大气科学] 0816[工学-测绘科学与技术] 0825[工学-航空宇航科学与技术]
基 金:supported by the National Key Research and Development Program of China[grant number 2017YFA060 4000] the China Meteorological Administration Special Public Welfare Research Fund[grant number GYHY201406001] the National Natural Science Foundation of China(NSFC)[grant number 91537108] the Natural Science Foundation of Jiangsu Province,China[grant number BK20160041] the U.S.Department of Energy’s BER Atmospheric System Research Program[grant number DE-SC00112704] the Six Talent Peak Project in Jiangsu,China[grant number 2015-JY-011] the 333 High-level Talents Training Project in Jiangsu[grant number BRA2016424] the NSFC[grant number 41305120]
摘 要:研究目的:介绍暖云降水之谜,总结湍流起伏和夹卷对云滴谱拓宽和暖雨形成过程的影响,包括观测、实验、模拟和理论方面取得的成果。重点阐述我国上世纪五六十年代在湍流起伏方面的突出成绩。重要结论:过饱和度、云滴数浓度、含水量和垂直速度等的起伏对凝结和碰并过程有显著影响。中国和俄罗斯科学家最早把随机凝结过程引入到云物理研究中。夹卷过程可能是暖云降水之谜的一个解。系统理论表明:湍流强度越大,云滴谱越宽。