Anomalously Wet Dry Seasons in Indonesia and Moisture Convergence Anomalies during The Cool Phase of Different ENSO Types Institut Teknologi Bandung Abstract Dry season in Indonesia typically occurs from June to September, overlapping with the Indian Summer Monsoon (ISM) period, during which India sub-continent and its surroundings receive large amount of moisture transported from oceans in the Indo-Pacific region. However, there have been years with anomalously wet dry season, more commonly known as ^wet dry-season^ (WDS) among the media, in Indonesia. On the other hand, the Meteorology, Climatology, and Geophysical Agency of Indonesia (BMKG) officially defines seasonal rainfall variations by three categories i.e., above normal (AN), normal (N), below normal (BN). However, there is no clear definition of WDS referring to AN criteria of the dry-season rainfall. This study attempts to make clear definition of WDS by applying the criteria of AN, N, and BN the seasonal rainfall variations on gridded rainfall data. Moisture convergence anomalies associated with identified years of wet-dry season are also analyzed. Keywords: Rainfall in dry season, anomalous wet-dry season identification, ENSO, moisture transport convergence Topic: Atmospheric Sciences |
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