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中国农学通报 ›› 2017, Vol. 33 ›› Issue (18): 94-102.doi: 10.11924/j.issn.1000-6850.casb16060108

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

2016年春运期间一次寒潮天气过程诊断分析

马严枝,李娟,李新生,闫慧,张磊,赵海英   

  1. 山西省气象台 030006,山西省气象台 030006,山西省气象台 030006,山西省气象台 030006,山西省气象台 030006,山西省气象台 030006
  • 收稿日期:2016-06-21 修回日期:2016-12-18 接受日期:2016-12-21 出版日期:2017-06-28 发布日期:2017-06-28
  • 通讯作者: 马严枝
  • 基金资助:
    中国气象局预报员专项项目“多源资料在山西暴雪天气预报中的应用技术研究”(CMAYBY2016-011)。

Diagnosis Analysis of a Cold Wave Weather Process

  • Received:2016-06-21 Revised:2016-12-18 Accepted:2016-12-21 Online:2017-06-28 Published:2017-06-28

摘要: 利用常规气象观测资料、NECP/NCAR1°×1°再分析资料和探空资料,应用天气学分析和动力气象学诊断方法,对2016年1月21~24日山西寒潮、大风和降雪过程的影响系统配置、冷空气移动路径和高低空环流形势演变进行了诊断分析,并对大风和降雪主要成因进行了分析。结果表明:此次寒潮过程属于“横槽型”,500hPa上贝加尔湖东部的冷涡引导冷空气,沿西北偏西路径进入山西,以及地面冷高压南下是寒潮爆发的原因。850 hPa存在强盛的冷平流,是产生寒潮天气的主要原因。但由于冷空气移动路径偏西,冷高压主体偏北,造成本次降温幅度只有个别站点突破历史极值。水汽条件较差,所有降水过程较弱;地面正负3h变压差达10hPa,利于产生变压风,造成大风天气。

关键词: 甜菜, 甜菜, ISSR, 品种鉴定, 引物筛选

Abstract: By using the conventional meteorological observation data, NCEP/NCAR 1°× 1° reanalysis data and radiosonde data, adopting synoptic meteorology principle and methods, the influenced system configuration, cold air path and changing circumstance of the high and low air circulation, and physical characteristics of the cold wave weather process in Shanxi during the spring festival on January 21-24, 2016 were analyzed. The results showed that: this was a “horizontal groove type” cold wave process, the cold eddy in the east of Lake Baikal of 500 hPa guiding the cold air, and the cold air path belonged to the west by northwest, and strengthening south of the ground cold high induced the cold wave in Shanxi; the main cause of temperature drop was the puissant cold advection in 850 hPa; but due to the cold air moving path by west, and cold high pressure subject was north, caused by the cooling rate only individual site break through the historical extreme value. Water vapor condition was bad, so precipitation was less; plus-minus surface variation in 3 hours was up to 10 hPa, which was beneficial to produce allobaric wind, then formed the strong wind weather.

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