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中国农学通报 ›› 2015, Vol. 31 ›› Issue (20): 213-218.doi: 10.11924/j.issn.1000-6850.casb15040040

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

贵州冻雨初终日的气候变化及其异常年环流特征

宋 丹1,唐延婧1,白 慧2,庞庆兵3   

  1. (1贵州省气象服务中心,贵阳 550002;2贵州省气候中心,贵阳 550002;3贵州省气象台,贵阳 550002)
  • 收稿日期:2015-04-06 修回日期:2015-07-01 接受日期:2015-05-08 出版日期:2015-07-28 发布日期:2015-07-28
  • 通讯作者: 宋丹
  • 基金资助:
    黔科合重大专项字(2011)6003号和黔科合院士站(2014)4010号

Climate Change and Abnormal Years’ Circulation Characteristics of the Beginning and Ending Dates of Freezing Rain in Guizhou

  1. Song Dan1, Tang Yanjing1, Bai Hui2, Pang Qingbing3(1Meteorological Service Center of Guizhou Province, Guiyang 550002;2Guizhou Climate Center, Guiyang 550002; 3Guizhou Meteorological Observatory, Guiyang 550002)
  • Received:2015-04-06 Revised:2015-07-01 Accepted:2015-05-08 Online:2015-07-28 Published:2015-07-28

摘要: 为了补充和完善贵州冻雨在初(终)日以及相关高度场等方面的特征,利用1964年10月—2014年4月贵州省冻雨观测资料和NCEP/NCAR再分析资料,分析了冻雨初日、终日和冻雨期的气候特征,及其高相关季节异常年北半球500 hPa的高度距平场特征。结果表明:冻雨初日渐晚、终日渐早、冻雨期渐短;初日多出现在11月中旬—12月上旬,终日多出现在3月;冻雨初日异常年夏季北半球高度距平场主要表现为中高纬度槽脊强度的异常,反映为北美大槽强度相反的变化特征;冻雨终日冬季高度距平场反映为高纬度极涡中心位置和强度的变化;冻雨期异常年则表现为不同的遥相关型,偏少年反映为PJ波列,偏多年表现为ANA、NEP和AWE并存,在实际业务中可以结合该信号特征对其进行长期预测。

关键词: 钙素化肥, 钙素化肥, 大蒜, 产量, 叶片性状

Abstract: The paper aims to supplement and improve the features of the freezing rain in early (end) days and the height field in Guizhou, by using the observation data and NCEP/NCAR reanalysis data of freezing rain in Guizhou from October 1964 to April 2014, this article researched climate characteristics of freezing rain’s beginning date, ending date and freezing rain period, also the features of northern hemisphere’s height anomaly fields at 500 hPa of anomalous years in high correlated seasons. Results showed that: the beginning dates of freezing rain were gradually became later, the periods were became short, and the ending dates did not change significantly. The beginning dates usually appeared between mid November to early December, and the ending dates appeared in the March. In summers of years with abnormal beginning dates of freezing rain, the northern hemisphere’s height anomaly mainly presented the characteristic of trough-ridge strength’s abnormal in mid-high latitude, with changes opposite the intensity of north American trough; in winters of years with abnormal ending dates of freezing rain, height anomaly featured mainly by the position and intensity variability of the polar vortex in high latitude. Freezing rain period showed different teleconnection, as the PJ wave appearing in shorter years, and ANA, NEP and AWE coexisting in longer years. Combined with these characteristics, the beginning & ending date and period of freezing rain could be long-term predicted in practice.