ZHOU Jing-shi,WANG Dong-hai.The Vertical Structure of Cloud in the Qinling-Daba Mounts[J].Journal of Chengdu University of Information Technology,2016,(05):523-530.
秦巴山区云垂直结构分析
- Title:
- The Vertical Structure of Cloud in the Qinling-Daba Mounts
- 文章编号:
- 2096-1618(2016)05-0523-08
- 关键词:
- 气象学; 云微物理; 秦巴山区; 云垂直结构特征; 水汽-云-降水相互关系
- Keywords:
- inling-Daba Mounts; vertical structure of cloud; the relationship of vapor; cloud and precipitation
- 分类号:
- P463.21+3
- 文献标志码:
- A
- 摘要:
- 为探讨秦巴地区降水与云垂直结构特征之间的关系,利用近8年(2006年7月~2014年6月)的CloudSat数据,通 过归一化等频率高度图(NCFAD)统计方法统计了各物理量各层的发生频数并对秦巴山区降水云的雷达反射率、云类 型、云微物理量及热力参数的垂直分布特征进行了研究,结果表明:(1)秦巴山区降水云以层云和雨层云为主,夏季 对流云的垂直发展最旺盛;(2)降水云雷达回波随高度先增加后减少,夏季具有典型强降水回波特征,春秋季呈一般 降水回波特特征,即回波大值区同时出现几个极值,冬季降水回波特征不显著;(
- Abstract:
- To discuss the relationship between the precipitation and cloud vertical structure over the Qinling-Daba Mounts(DQM), the research analyzed with the CloudSat data during the period from July 2006 to June 2014 presents the vertical distribution of the radar reflectivity, cloud type, the microphysical parameters and the thermal parameters by using NCFAD statistical methods to calculate the occurrence frequency of each physical quantity in each layer. The results show that, (1)the main type of precipitation-cloud in DQM are stratus and nimbostratus, the deep convective clouds fully develop in vertical in summer;(2)the radar reflectivity of precipitation-cloud increase and then decrease with height and shows typical heavy precipitation echo characteristics in summer, verage precipitation echo characteristics in autumn and springseveral extreme values occur at same time, characteristics of the precipitation echo was not significant in winter;(3)Ice cloud particles are mainly distributed in 3-8 km, particle concentration increases with height; liquid cloud particles concentration in 2-4 km, the particle concentration decreases with height; (4)Thermal structure varies little in different seasons, and the atmosphere seasonis convectivestab.
参考文献/References:
[1] 王标.气候变化研究中大气垂直结构探测评述[J].大气与环境光学学报,2011,6(1):2-10.
[2] 李积明,黄建平,衣育红,等.利用星载激光雷达资料研究东亚地区云垂直分布的统计特征[J].大气科
学,2009,33(4):698-707.
[3] Jackob C,Klei S A.The role of vertically varying cloud fraction in the parametrization of
microphysical processes in theECWMF model[J].Quart J Roy Meteor Soc,1999,125(555):941-965.
[4] 张中波,仇财兴,王治平,等.一次积层云混合云系人工增雨作业的观测分析[J].气象科技,2014,42
(5):897-905.
[5] 李玉文,王盘兴,杜继稳,等.秦巴山区暴雨及其诱发地质灾害的特征分析[J].陕西气象,2007,(1):21-25.
[6] 杨波,张勃,安美玲,等.1961-2011年秦巴山区极端降水事件的时空分布特征分析[J].水土保持研
究,2014,21(1):110-116.
[7] 朱梅,肖天贵,余兴,等.秦巴谷底夏季降水的时空分布特征分析[J].气象科技,2014,42(4):664-670.
[8] 毕宝贵,刘月巍,李泽椿.秦岭大巴山地形对陕南强降水的影响[J].高原气象,2006,25(3):495-494.
[9] 马学谦,陈跃,张国庆,等.X波段双偏振雷达对不同坡度地形云探测个例分析[J].干旱气象,2015,33
(4):675-683.
[10] 郑国光,陈跃,陈添宇,等.祁连山夏季地形云综合探测试验[J].地球科学进展,2011,26(10):1057-1070.
[11] 王德旺,刘黎平,仲凌志,等.毫米波雷达资料融化层亮带特征的分析及识别[J].气象,2012,38(6):712-
721.
[12] 马占山,刘奇俊,秦琰琰,等.云探测卫星cloudsat[J].气象,2008,34(8):104-111
[13] 赵艳风,王东海,尹金方.基于CloudSat资料的青藏高原地区云微物理特征分析[J].热带气象学
报,2014,(2):239-248.
[14] 尹金方,王东海,翟国庆,等.基于星载云雷达资料的东亚大陆云垂直结构特征分析[J].气象学
报,2013,71(1):121-133.
[15] 韩丁,严卫,叶晶,等.基于CloudSat卫星资料分析东太平洋的云、降水和热力特征[J].大气科
学,2013,37(3):691-704.
[16] 廖菲,洪延超,郑国光.影响云和降水的动力、热力与微物理因素的研究概述[J].气象,2006,32(11):3-
11.
[17] 陈英英,周毓荃,毛节泰,等.利用FY-2C静止卫星资料反演云粒子有效半径的试验研究[J].气
象,2007,33(4):29-34.
[18] 杨大生,王普才.中国地区夏季6~8月云水含量的垂直分布特征[J].大气科学,2012,36(1):89-101.
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备注/Memo
收稿日期:2016-02-20 基金项目:财政部/科技部行业专项资助项目(GYHY201306005); 国家自然科学基金重点资助项目(91437221)