四川地区夏季旱涝与西太平洋副热带高压的关系

Relationship between the Drought and Flood Intensity in Sichuan Area in Summer and West Pacific Subtropical High

  • 摘要: 利用近46年西太平洋副热带高压特征指数资料、四川地区123个测站的逐日降水资料集及NCEP\NCAR再分析资料,研究了四川地区夏季旱涝事件的空间分布特征及其与西太副高的关系。结果表明,四川盆地东西部经常出现"西旱东涝"或者"西涝东旱"的异常特征。西太平洋副热带高压的脊线、北界位置与四川盆地东(西)部区的旱涝之间存在很高正(负)相关关系。西太平洋副热带高压南北位置的异常变化对应着东亚地区大气环流的异常变化,从而影响四川盆地东部区及四川盆地西部区的旱涝变化。

     

    Abstract: Based on the monthly west pacific subtropical high indexes in summer,the daily precipitation data in summer collected by 123 stations from 1961 to 2007 and the monthly NCEP/NCAR reanalysis data,the correlation coefficients between them and the features of drought-flood coexistence in the west and east of Sichuan-Chongqing basin in summer are studied.The results indicate that the correlation coefficients between the ridge,north boundary of West Pacific Subtropical High and drought and flood events in East Sichuan Basin,West Sichuan Basin is markedly.The anomaly latitudinal position of West Pacific Subtropical High has significant impact on the atmospheric circulation in East Asia and drought and flood events in East Sichuan Basin and West Sichuan Basin in summer.

     

/

返回文章
返回