| 注册
首页|期刊导航|气象|导致区域性雷暴大风天气的云型分类及统计特征分析

导致区域性雷暴大风天气的云型分类及统计特征分析

方翀 郑永光 林隐静 朱文剑

气象Issue(8):905-915,11.
气象Issue(8):905-915,11.DOI:10.7519/j.issn.1000-0526.2014.08.001

导致区域性雷暴大风天气的云型分类及统计特征分析

Classification and Characteristics of Cloud Patterns Triggering Regional Thunderstorm High Winds

方翀 1郑永光 1林隐静 1朱文剑1

作者信息

  • 1. 国家气象中心,北京 100081
  • 折叠

摘要

Abstract

Based on the satellite data,observational data of upper-air and significant weather report from 2005 to 2011,the weather situation at 500 hPa and the cloud patterns of 18 processes of thunderstorm high winds are classified and analyzed.The development of cloud patterns can be divided into 4 stages:initial, growing,mature and dissipating.The brightness temperature difference between IR1 channel and water vapor channel is mostly negative,and the number’s decreasing indicates that the severe convective clouds are still developing.We need to pay more attention to the right part or the right single-cell storm of the elongated strong convective clouds when we monitor and forecast the cloud system of thunderstorm high winds,especially the low TBB areas,the high TBB gradient part and the area coordinating with the nega-tive area of IR1 and WV channel brightness temperature difference.Quantitative statistical analysis of the characteristic value are made on the basis of subjective analysis,and we get the distribution of the infrared brightness temperature,water vapor brightness temperature,channel brightness temperature difference and infrared brightness temperature gradient near the sites observing the thunderstorm high winds.We discover that the majority of thunderstorm high winds often take place during the period when the infrared brightness temperature develops from a sharp decline to a gentle decline and at the time point when the channel brightness temperature gently slows down or becomes stable.Moreover,most examples are near the time period when the channel brightness temperature difference changes from positive to negative,and at the point when the infrared brightness temperature gradient approaches the largest area or begins to decline.

关键词

雷暴大风/云型/红外亮温/通道亮温差/亮温梯度

Key words

thunderstorm high winds/cloud pattern/infrared brightness temperature/brightness tempera-ture difference/brightness temperature gradient

分类

天文与地球科学

引用本文复制引用

方翀,郑永光,林隐静,朱文剑..导致区域性雷暴大风天气的云型分类及统计特征分析[J].气象,2014,(8):905-915,11.

基金项目

公益性行业(气象)科研专项(GYHY201206003)、国家重点基础研究计划(973计划)项目(2013CB430106)、国家自然科学基金项目(41375051)共同资助完成 ()

气象

OA北大核心CSCDCSTPCD

1000-0526

访问量0
|
下载量0
段落导航相关论文