高娜1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2,孙健1,3,王春学4,郑广芬1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2,杨建玲1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2
GAO Na1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2, SUN Jian1,3, WANG Chunxue4, ZHENG Guangfen1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2, YANG Jianling1,2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2[Author]) AND 1[Journal]) AND year[Order])" target="_blank">2
摘要:
利用1961—2016年NCEP/NCAR逐月再分析资料和宁夏20个气象台站逐日降水观测资料,分析宁夏春季降水异常年东亚副热带急流异常特征,并简要分析可能影响原因。结果表明:春季降水异常年同期及前期,副热带纬向风均存在空间结构异常,且在110°E—160°E异常年反位相特征表现更显著。在降水异常偏少(多)年同期及前期,水平及垂直方向上均存在东亚副热带急流区西风增强(减弱),但前期反位相对应关系不如同期明显;建立的春季东亚副热带急流指数与宁夏春季降水呈显著正相关,春季东亚副热带急流指数为负(正)异常时,东亚大槽较常年加深(略浅),宁夏地区受西北(南支)气流影响,850 hPa风场也表现为偏北风(偏南风)距平,不利于(有利于)形成降水。