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| 2008年初江苏暴雪天气的诊断分析 | |
| 引用本文： | 王桂臣,张红华,姜有山,王伯盛,陈飞.2008年初江苏暴雪天气的诊断分析[J].气象科学,2010,30(1):60-66. |
| 作者姓名： | 王桂臣 张红华 姜有山 王伯盛 陈飞 |
| 作者单位： | 1. 连云港市气象局,江苏连云港,222006;南京信息工程大学,气象灾害省部共建教育部重点实验室,南京,210044 2. 连云港市气象局,江苏连云港,222006 3. 东海县气象局,江苏东海,222300 |
| 基金项目： | 国家科技支撑计划课题，江苏省连云港市科学技术局项目 |
| 摘 要： | 用2008年1月25—29日NCEP/NCAR一日四次全球再分析资料对1月25—29日江苏省大范围强降雪过程的天气背景、散度场、水汽通量的流函数与势函数、视热源与视水汽汇以及Q矢量等物理量进行了分析,并进行了南北地区的对比。结果表明:(1)200 hPa与850 hPa的散度差值场,与降雪落区有较好的对应关系;(2)沿江和苏南地区明显的水汽辐合,配合北方冷空气的向南侵入,是造成江淮流域持续暴雪的重要原因之一;(3)强降雪期间,非绝热加热对降雪产生重要影响,其中淮河以南降雪以对流性降雪为主,淮河以北地区以非对流性降雪为主;(4)非地转风造成的Q矢量辐合区主要位于850 hPa切变线附近,为强降雪提供了有利条件。 |
| 关 键 词： | 暴雪 水汽输送 非绝热加热 Q矢量 |
| 收稿时间： | 2008/10/7 0:00:00 |
Diagnostic analysis of heavy snow weather in Jiangsu province in winter of 2008 |
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| Wang Guichen,Zhang Honghua,Jiang Youshan,Wang Bosheng,Chen Fei.Diagnostic analysis of heavy snow weather in Jiangsu province in winter of 2008[J].Scientia Meteorologica Sinica,2010,30(1):60-66. | |
| Authors: | Wang Guichen Zhang Honghua Jiang Youshan Wang Bosheng Chen Fei |
| Institution: | Wang Guichen1,2 Zhang Honghua1,2 Jiang Youshan1 Wang Bosheng3 Chen Fei1 (1 Lianyungang Meteorological Bureau,Jiangsu Lianyungang 222006,China) (2 Key Laboratory of Meteorological Disaster of Ministry of Education,NUIST,Nanjing 210044,China) (3 Donghai Meteorological Bureau,Jiangsu Donghai 222300,China) |
| Abstract: | Using NCEP/NCAR reanalysis data during 25-29 Jan. 2008,we have analyzed the physical quantities including the circulations for weather background, divergence field, vertical velocity field, streamfunction along with the potential velocity of water vapor transport, and the Q vectors during the heavy snow process as observed in Jiangsu province. The comparison of features of those physical quantities in southern part of Jiangsu, where the snow center is located, with those in the northern part of Jiangsu has been made. Our results have demonstrated that the falling area of snow can be identified well by the positive value of differences of the divergence of wind at 200 hPa with that at 850 hPa, which is meaningful for us to predict the place where the snowstorm will occur. The significant moisture convergence, along with the anomalies of cold air that appear around Yangtze River and southern of Jiangsu, is one of the important factors determining the continuous heavy snowfall over the Yangtze-Huaihe Valley. The Q vector convergence area caused by ageostrophic wind which is located in shear line at 850 hPa possibly provide a favorable condition for this heavy snowfall process. |
| Keywords: | Heavy snow Water vapor Diabatic heating Q vector |
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