Characterizing every year during the 120 year interval 1871 -1990 as a year of El Nin หo (EN), or Southern Oscillation minimum (SO), or equatorial eastern Pacific sea-surface temperature (SST) warm (W) or cold (C) episode or none (non-events), the corresponding summer monsoon rainfall departures for
Extremes of the Indian summer monsoon rainfall, ENSO and equatorial Indian Ocean oscillation
โ Scribed by Gadgil, Sulochana
- Book ID
- 119662768
- Publisher
- American Geophysical Union
- Year
- 2004
- Tongue
- English
- Weight
- 247 KB
- Volume
- 31
- Category
- Article
- ISSN
- 1944-8007
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๐ SIMILAR VOLUMES
## Abstract We examine the relationship between the state of the equatorial Indian Ocean, ENSO, and the Indian summer monsoon rainfall using data from 1881 to 1998. The zonal wind anomalies and SST anomaly gradient over the equatorial Indian Ocean are used as indices that represent the condition of
Association between the all-India summer monsoon (June to September) rainfall and an index of the Southern Oscillation (SO) is studied in relation to the vagaries of the monsoon rainfall and the seasonal characteristics of the SO. The Southern Oscillation index (SOI) used is the difference of normal