Comparison of the Structure and Evolution of Intraseasonal Oscillations Before and After Onset of the Asian Summer Monsoon

High-resolution satellite-derived data and NCEP-NCAR reanalysis data are used to investigate intraseasonal oscillations (ISO) over the tropical Indian Ocean.A composite evolution of the ISO life cycle is constructed,including the initiation,development,and propagation of rainfall anomalies over the...

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Bibliographic Details
Published inActa meteorologica Sinica Vol. 27; no. 5; pp. 684 - 700
Main Author 齐艳军 张人禾 赵平 翟盘茂
Format Journal Article
LanguageEnglish
Published Heidelberg The Chinese Meteorological Society 01.10.2013
Chinese Academy of Meteorological Sciences,Beijing,100081
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ISSN0894-0525
2191-4788
DOI10.1007/s13351-013-0511-2

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Summary:High-resolution satellite-derived data and NCEP-NCAR reanalysis data are used to investigate intraseasonal oscillations (ISO) over the tropical Indian Ocean.A composite evolution of the ISO life cycle is constructed,including the initiation,development,and propagation of rainfall anomalies over the tropical Indian Ocean.The characteristics of ISO over the tropical Indian Ocean are profoundly different before and after the onset of the Indian summer monsoon.Positive precipitation anomalies before monsoon onset appear one phase earlier than those after monsoon onset.Before monsoon onset,precipitation anomalies associated with ISO first initiate in the western tropical Indian Ocean and then propagate eastward along the equator.After monsoon onset,convective anomalies propagate northward over the Indian summer monsoon region after an initial eastward propagation over the equatorial Indian Ocean.Surface wind convergence and air-sea interaction play critical roles in initiating each new cycle of ISO convection.
Bibliography:High-resolution satellite-derived data and NCEP-NCAR reanalysis data are used to investigate intraseasonal oscillations (ISO) over the tropical Indian Ocean.A composite evolution of the ISO life cycle is constructed,including the initiation,development,and propagation of rainfall anomalies over the tropical Indian Ocean.The characteristics of ISO over the tropical Indian Ocean are profoundly different before and after the onset of the Indian summer monsoon.Positive precipitation anomalies before monsoon onset appear one phase earlier than those after monsoon onset.Before monsoon onset,precipitation anomalies associated with ISO first initiate in the western tropical Indian Ocean and then propagate eastward along the equator.After monsoon onset,convective anomalies propagate northward over the Indian summer monsoon region after an initial eastward propagation over the equatorial Indian Ocean.Surface wind convergence and air-sea interaction play critical roles in initiating each new cycle of ISO convection.
QI Yanjun, ZHANG Renhe, ZHAO Ping, and ZHAI Panmao( Chinese Academy of Meteorological Sciences, Beijing 100081)
11-2277/P
tropical Indian Ocean; intraseasonal oscillation; Asian summer monsoon; onset
ISSN:0894-0525
2191-4788
DOI:10.1007/s13351-013-0511-2