干旱气象 ›› 2019, Vol. 37 ›› Issue (6): 906-915.

• 论文 • 上一篇    下一篇

鄂北春播期降水异常能量输送及成因分析

王晓玲1,高正旭2,王海燕1,陈赛男1,王艳杰1   

  1. 1.武汉中心气象台,湖北武汉430074;2.武汉区域气候中心,湖北武汉430074
  • 出版日期:2019-12-31 发布日期:2020-01-02
  • 通讯作者: 高正旭(1980— ),男,高级工程师,主要从事气候可行性论证、应用气象领域的研究. E-mail:gaozhengxu21@foxmail.com。
  • 作者简介:王晓玲(1978— ),女,高级工程师,主要从事中短期预报方法及灾害天气分析研究. E-mail:w_x_ling21@foxmail.com。

Analysis of Energy Transmission and Formation Cause of Precipitation Anomaly in Spring Sowing Period in Northern Hubei

WANG Xiaoling1, GAO Zhengxu2, WANG Haiyan1, CHEN Sainan1, WANG Yanjie1#br#

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  1. 1. Wuhan Central Meteorological Observatory ,Wuhan 430074, China;
    2. Wuhan Regional Climate Center, Wuhan 430074, China
  • Online:2019-12-31 Published:2020-01-02

摘要: 利用1981—2018年降水观测信息,结合NCEP再分析资料,采用合成诊断以及大气能谱方法,对比分析鄂北春播期降水异常天气成因。结果表明:降水偏少年副热带高压偏弱偏南,极涡偏弱,中纬度扰动动能表现为经向弱,纬向输送位置偏南,角动量以向南输送为主,南北能量交换弱,因而鄂北地区冷暖空气交汇不明显,对流层低层为辐散气流,不利于产生锋生动力。降水偏多年副热带高压和极涡均偏强,高原槽活动频繁,中纬度扰动动能表现为经向强,纬向输送位置偏北,角动量南北输送均明显,能量交换频繁,因而鄂北地区冷暖空气交汇明显,对流层低层为辐合气流,利于产生锋生动力。

关键词: 降水异常, 能量输送, 扰动动能, 角动量

Abstract: Based on precipitation observation information and NCEP reanalysis data during 1981-2018, the causes of abnormal precipitation in spring sowing period in northern Hubei Province were analyzed by using synthetic diagnostics and atmospheric energy spectrum methods. The results show that in abnormally less precipitation years, the subtropical high was weaker and its position was southerly, and the polar vortex was weaker too. The perturbation kinetic energy over mid-latitude was weak in meridional direction, while the zonal transfer position was southerly, and the angular momentum transferred obviously to the south, the energy exchange between north and south was weak. Thus the intersection of cold and warm air was not obvious over the north of Hubei, and it was divergent in the lower troposphere, which was not conducive to the frontogenesis. In abnormally more precipitation years, both the subtropical high and polar vortex were stronger, the plateau trough was more actively. The perturbation kinetic energy over mid-latitude was stronger in meridional direction, while the zonal transfer position was northerly,the angular momentum transferred obviously and the energy exchanged frequently between the south and north. Thus the intersection of cold and warm air was obvious over the north of Hubei, it was convergence in the lower troposphere, which was conducive to the frontogenesis.

Key words: precipitation anomalies, energy transfer, perturbation kinetic energy, angular momentum

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