海洋气象学

热带气旋“桑美(2006)”冰云微物理属性垂直分布规律*

  • 张蕾 ,
  • 史兰红 ,
  • 徐健 ,
  • 孙冉 ,
  • 赵兵科 ,
  • 陈勇航 ,
  • 王晓峰 ,
  • 王文彩 ,
  • 李梦 ,
  • 丁明月
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  • 1. 东华大学环境科学与工程学院, 上海 201620;
    2. 中国气象局上海台风研究所, 上海 200030;
    3. 中国海洋大学海洋环境学院, 山东 青岛 266100
张蕾(1979—), 女, 江苏省邳州市人 副研究员, 博士, 主要从事台风数值预报技术和非常规观测资料同化技术研究。E-mail: zhangl@mail.typhoon.gov.cn

收稿日期: 2013-09-25

  网络出版日期: 2016-05-27

基金资助

公益性行业科研专项(GYHY201406010); “十二五”国家科技支撑计划项目(2012BAC21B02); 国家自然科学基金项目(41175026)

Vertical distribution of ice cloud microphysical properties of tropical cyclone Saomai (2006)*

  • ZHANG Lei ,
  • SHI Lanhong ,
  • XU Jian ,
  • SUN Ran ,
  • ZHAO Bingke ,
  • CHEN Yonghang ,
  • WANG Xiaofeng ,
  • WANG Wencai ,
  • Li Meng ,
  • DING Mingyue
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  • 1. College of Environmental Science and Engineering, Donghua University, Shanghai 201620, China;
    2. Shanghai Typhoon Institute of China Meteorological Administration, Shanghai 200030, China;
    3. College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China

Received date: 2013-09-25

  Online published: 2016-05-27

Supported by

Meteorological Industry Research for Public Welfare (GYHY20140610); National Science and Technology Supporting Plan (2012BAC21B02); National Natural Science Foundation of China (41175026)

摘要

利用2006年8月3日—11日CloudSat卫星的云反演资料, 探讨了热带气旋“桑美(2006)”在形成期、发展成熟期和减弱期不同部位云中冰粒子的垂直分布规律。结果表明: 星载雷达扫过热带气旋“桑美(2006)”不同部位时, 云中冰粒子主要分布在5~16.5km高度; 冰粒子等效半径随高度递增而递减, 大值区主要分布在冰云下部; 冰粒子数浓度随高度递增而递增, 大值区主要分布在冰云上部; 冰水含量的垂直分布呈单峰或双峰特征; 星载雷达监测到的该热带气旋不同部位的冰粒子等效半径、冰粒子数浓度、冰水含量的最大值分布范围分别为107.9~177.7μm、123.8~827.9粒•L-1、211~2858mg·m-3, 最大值出现高度存在差异。

本文引用格式

张蕾 , 史兰红 , 徐健 , 孙冉 , 赵兵科 , 陈勇航 , 王晓峰 , 王文彩 , 李梦 , 丁明月 . 热带气旋“桑美(2006)”冰云微物理属性垂直分布规律*[J]. 热带海洋学报, 2016 , 35(3) : 30 -40 . DOI: 10.11978/2013119

Abstract

Using the retrieved data from CloudSat during August 3-11, 2006, the vertical distributions of ice particles in the clouds of different parts of tropical cyclone (TC) Saomai (2006) were analyzed, in their formation period, development-to- mature period and weakening period. The results are as follows. When the space-borne radar swept through different parts of TC Saomai (2006), ice particles in the clouds mainly distributed from the height of 5 to 16.5 km. The ice particle effective radius (re) reduced with increasing altitude and the large particles were mainly concentrated at the bottom of the ice clouds. The ice particle number concentration (Cin) increased with increasing altitude and large particles were mainly at the top of the ice clouds; the vertical distribution of the ice water content (Ciw) had a shape of unimodal or bimodal. The heights of the maximum re, Cin and Ciw were different from each other, and the ranges of the maximum what for re, Cin and Ciw were 107.9~177.7 μm, 123.8~827.9 L-1 and 211~2858 mg•m-3, respectively.

参考文献

1 段云霞, 邵爱梅, 杨毅, 2010. 利用双多普勒雷达资料对一次台风流场结构的分析[J]. 高原气象, 29(1): 187-196. DUAN YUNXIA, SHAO AIMEI, YANG YI, et al, 2010. Analysis on three-dimension wind fields for a typhoon process using dual- Doppler radar[J]. Plateau Meteorology, 29(1): 187-196 (in Chinese).
2 傅云飞, 宇如聪, 徐幼平, 等, 2003. TRMM测雨雷达和微波辐射成像仪对两个中尺度特大暴雨降水结构的观测分析研究[J]. 气象学报, 61(4): 421-431. FU YUNFEI, YU RUCONG, XU YOUPING, et al, 2003. Analysis on precipitation structures of two heavy rain cases bu using TRMM PR and IMI[J]. Acta Meteorologica Sinica, 61(4): 421-431 (in Chinese).
3 傅云飞, 刘栋, 王雨, 等, 2007. 热带测雨卫星综合探测结果之“云娜”台风降水云与非降水云特征[J]. 气象学报, 65(3): 316-328. FU YUNFEI, LIU DONG, WANG YU, et al, 2007. Characteristics of precipitating and non-precipitating clouds in typhoon Ranan as viewed by TRMM combined mieasurements[J]. ATCA Meteoroogica Sinica, 65(3): 316-328 (in Chinese).
4 何会中, 程明虎, 周凤仙, 2006. 0302号(鲸鱼)台风降水和水粒子空间分布的三维结构特征[J]. 大气科学, 30(3): 491-503. HE HUIZHONG, CHENG MINGHU, ZHOU FENGXIAN, 2006. 3D structure of rain and cloud hydrometeors for typhoon Kujira (0302)[J]. Chinese Journal of Atmospheric Sciences, 30(3): 491-503 (in Chinese).
5 黄荣辉, 陈光华, 2007. 西北太平洋热带气旋移动路径的年际变化及其机理研究[J]. 气象学报, 65(5): 683-694. HUANG RONGHUI, CHEN GUANGHUA, 2007. Research on interannual variations of tracks of tropical cyclones over Northwest Pacific and their physical mechanism[J]. Acta Meteorologica Sinica, 65(5): 683-694 (in Chinese).
6 李积明, 黄建平, 衣育红, 等, 2009. 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, 33(4): 698-707. LI JIMING, HUANG JIANPING, YI YUHONG, et al, 2009. Analysis of vertical distribution of cloud in East Asia by space-based lidar data[J]. Chinese Journal of Atmospheric Sciences, 33(4): 698-707 (in Chinese).
7 马占山, 刘奇俊, 秦琰琰, 等, 2008. 云探测卫星CloudSat[J]. 气象, 34(8): 104-111. MA ZHANSHAN, LIU QIJUN, QIN YANYAN, et al, 2008. Introductions to a new type cloud detecting satellite - CloudSat[J]. Meteorological Monthly, 34(8): 104-112 (in Chinese).
8 王新利, 唐传师, 刘显通, 等, 2007. 利用TRMM卫星资料分析“桑美(2006)”台风云系特征[J]. 气象与减灾研究, 30(3): 7-11. WANG XINLI, TANG CHUANSHI, LIU XIANTONG, et al, 2007. Cloud characters of typhoon Saomai on the TRMM satellite data[J]. Meteorology and Disaster Reduction Research, 30(3): 7-13 (in Chinese).
9 夏秋萍, 王鹤祥, 陈子昂, 等, 2006. 用 TRMM卫星探测资料对“卡努”台风云系不同阶段特征的分析[J]. 海洋预报, 23(4): 28-36. XIA QIUPING, WANG HEXIANG, CHEN ZIANG, et al, 2006. Analysis of typhoon Khnun cloud characteristics in different stages by using TRMM[J]. Marine Forecasts, 23(4): 28-36 (in Chinese).
10 赵姝慧, 周毓荃, 2010. 利用多种卫星研究台风“艾云尼”宏微观结构特征[J]. 高原气象, 29(5): 1254-1260. ZHAO SHUHUI, ZHOU YUQUAN, 2010. Research on macro-micro structures of typhoon ‘Ewiniar’ using a variety of satellites[J]. Plateau Meteorology, 29(5): 1254-1260 (in Chinese).
11 周毓荃, 赵姝慧, 2008. CloudSat卫星以及在天气和云观测分析中的应用[J]. 南京气象学院学报, 31(5): 603-614. ZHOU YUQUAN, ZHAO SHUHUI, 2008. CloudSat satellite and its application in weather and cloud observation[J]. Journal of Nanjing Institute of Meteorology, 31(5): 603-614 (in Chinese).
12 BLACK R A, HALLETT J, 1986. Observations of the distribution of ice in hurricanes[J]. Journal of the Atmospheric Sciences, 43(8): 802-822.
13 BLACK R A, HALLETT J, 1999. Electrification of the hurricane[J]. Journal of the Atmospheric Sciences, 56(12): 2004-2028.
14 DURDEN S L, TANELLI S, DOBROWALSKI G, 2009. CloudSat and a-train observations of tropical cyclones[J]. Open Atmospheric Science Journal, 3(1): 80-92.
15 HOUZE R A, MARKS F D, BLACK R A, 1992. Dual-aircraft investigation of the core of hurricane Norbert, Part Ⅱ: mesoscale distribution of ice particles[J]. Journal of the Atmospheric Sciences, 49(11): 943-62.
16 HUANG JIANPING, MINNIS P, LIN BING, et al, 2005. Advanced retrievals of multilayered cloud properties using multispectral measurements[J]. Journal of Geophysical Research: Atmospheres (1984-2012), 110: D15.
17 HUANG JIANPING, MINNIS P, LIN BING, et al, 2006. Determination of ice water path in ice-over-water cloud systems using combined MODIS and AMSR-E measurements[J]. Geophysical Research Letters, 33(21): L21801.
18 LI WEIBIAO, WANG DONGXIAO, LEI TING, et al, 2011. High-frequency atmospheric variability over South China Sea as depicted by TRMM and QuikSCAT[J]. Acta Oceanologica Sinica, 30(2): 46-52.
19 PENG SHIQIU, QIAN YUKUN, LAI ZHIJUAN, et al, 2014. On the mechanisms of the recurvature of super typhoon Megi[J]. Scientific Reports, 4(12): 4451.
20 WANG XIN, ZHOU WEN, LI CHONGYIN, et al, 2012. Effects of the east Asian summer monsoon on tropical cyclone genesis over the South China Sea on an interdecadal time scale[J]. Advances in Atmospheric Sciences, 29(2): 249-262.
21 WANG XIN, ZHOU WEN, LI CHONGYIN, et al, 2014. Comparison of the impact of two types of El Niño on tropical cyclone genesis over the South China Sea[J]. International Journal of Climatology, 34(8): 2651-2660.
22 WU GUOXIONG, REN SULING, XU JIANMIN, et al, 2013. Impact of tropical cyclone development on the instability of South Asian high and the summer monsoon onset over bay of Bengal[J]. Climate Dynamics, 41(9/10): 2603-2616.
23 XU XIANGDE, PENG SHIQIU, YANG XIANGJING, et al, 2013. Does warmer China land attract more super typhoons?[J]. Scientific Reports, 3: 1522-1522.
24 YANG LEI, DU YAN, XIE SHANGPING, et al, 2012a. An interdecadal change of tropical cyclone activity in the South China Sea in the early 1990s[J]. Chinese Journal of Oceanology and Limnology, 30(6): 953-959.
25 YANG LEI, WANG DONGXIAO, PENG SHIQIU, et al, 2012b. Comparison between MM5 simulations and satellite measurements during typhoon Chanchu (2006) in the South China Sea[J]. Acta Oceanologica Sinica, 31 (2): 33-44.
26 YUAN JINNAN, WANG DONGXIAO, LIU CHUNXIA, et al, 2007a. The characteristic differences of tropical cyclones forming over the western North Pacific and the South China Sea[J]. Acta Oceanologica Sinica, 26(4): 29-43.
27 YUAN JINNAN, WANG DONGXIAO, WAN QI LIN, et al, 2007b. A 28-year climatological analysis of size parameters for Northwestern Pacific tropical cyclones[J]. Advances in Atmospheric Sciences, 24(1): 24-34.
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