昌都地区汛期降水与ENSO事件的关系
Analysis of Precipitation in Flood Season in Changdu during ENSO Events
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摘要: 利用昌都地区7站1980~2010年逐日、逐月降水资料与NCEP再分析资料,对昌都地区汛期(5~9月)降水进行分析,分析结果表明:昌都地区汛期降水在厄尔尼诺-南方涛动(NESO)事件的不同阶段存在显著差异,在ENSO发展阶段昌都地区汛期降水除八宿县外,各地均偏少。影响逐月降水的原因在于降水日数的变化,降水偏多月份中雨与大雨的降水日数增多,大雨日数增加明显;降水偏少月份,中雨与小雨降水日数偏少。对ENSO发展阶段和常年的大气环流对比得出,南亚高压偏东是影响汛期降水偏少的主要原因。Abstract: This paper analyzed the variations of meteorological elements during the flood season (May to September), by using the daily and monthly precipitation and NCEP reanalysis data from 1980~2010 from the 7 meteorological stations in Changdu. The results show that there is distinguished difference of precipitation during the flood season in Changdu between different stages of an El Nino-Southern Oscillation (NESO) event. The precipitation has reduced during the development stage of ENSO in the flood season in Changdu, except for Basu station. The variations of numbers of days with precipitations are contributed to monthly precipitation. The number of days of moderate and heavy rain increased in the months when the precipitation is high, whereas the number of days of moderate and light rain decreased in the months when the precipitation is low.The low precipitation is mainly caused by the South Asia high exhibiting the east, by comparing the atmospheric circulation between the regular year and the year with ENSO