摘要
Historical La Nia events since 1950 are divided into Eastern Pacific(EP) type and Central Pacific(CP) type,and the SSTA developing features as well as the different responses of the tropical atmosphere are further analyzed by using multiple datasets.Classification of different types La Nia is based on the normalized Ni o3 and Ni o4 indices and the SSTA distribution pattern during the mature phase.The minimum negative SSTA for CP La Nia is located over the equatorial central Pacific near the dateline,more westward than that of EP La Nia.It has stronger intensity and larger east-west zonal difference of SSTA over the equatorial Pacific than EP La Nia.Influenced by the different SSTA distribution pattern,CP La Nia induces more westward location of the anomalous sinking motion and the anomalous low-level divergent and high-level convergent winds over the equatorial eastern Pacific.The different response of the tropical atmospheric circulation between EP and CP La Nia is more significant in the upper troposphere than in the lower troposphere.However,the tropical precipitation patterns during the mature phase of EP and CP La Nia are much similar,except the less(more) precipitation over the equatorial central Pacific(eastern Indian Ocean-western Pacific) during CP La Nia than during EP La Nia.
Historical La Nifia events since 1950 are divided into Eastern Pacific （EP） type and Central Pacific （CP） type, and the SSTA developing features as well as the different responses of the tropical atmosphere are further analyzed by using multiple datasets. Classification of different types La Nina is based on the normalized Nifio3 and Nifio4 indices and the SSTA distribution pattern during the mature phase. The minimum negative SSTA for CP La Nina is located over the equatorial central Pacific near the dateline, more westward than that of EP La Nifia. It has stronger intensity and larger east-west zonal difference of SSTA over the equatorial Pacific than EP La Nifia. Influenced by the different SSTA distribution pattern, CP La Nifia induces more westward location of the anomalous sinking motion and the anomalous low-level divergent and high-level convergent winds over the equatorial eastern Pacific. The different response of the tropical atmospheric circulation between EP and CP La Nifia is more significant in the upper troposphere than in the lower troposphere. However, the tropical precipitation patterns during the mature phase of EP and CP La Nina are much similar, except the less （more） precipitation over the equatorial central Pacific （eastern Indian Ocean-western Pacific） during CP La Nina than during EP La Nina.
基金
supported by the Young Scientists Fund of the National Natural Science Foundation of China(41005038 and 41065004)
the Chinese Public Sector(Meteorology) Research and Special Project (GYHY200906016)
the National Key Technology Research and Development Program of China(2009BAC51B01)
关键词
热带大气环流
拉尼娜事件
反应
类型
风情
赤道东太平洋
赤道太平洋
海温异常
La Nina, Eastern Pacific （EP） type, Central Pacific （CP） type, tropical atmosphere, Walker circulation, precipitation
