Blocking highs over Asia and monsoon droughts over India
Severe summer droughts of the Indian subcontinent have been found to accompany prolonged ‘breaks’ in the south-west monsoon. Data from the years of severe drought suggest that the associated breaks were due to upper tropospheric blocking ridges over East Asia. We present here a model for the evoluti...
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Veröffentlicht in: | Nature (London) 1981-01, Vol.289 (5795), p.271-273 |
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Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | Severe summer droughts of the Indian subcontinent have been found to accompany prolonged ‘breaks’ in the south-west monsoon. Data from the years of severe drought suggest that the associated breaks were due to upper tropospheric blocking ridges over East Asia. We present here a model for the evolution of two such blocking ridges: the East Asia (EABR) and the West Asia (WABR). Apparently an intense WABR—the initiator of the monsoon break—precedes the formation of the EABR. This cycle could be a way of predicting years of intense drought or monsoon activity. |
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ISSN: | 0028-0836 1476-4687 |
DOI: | 10.1038/289271a0 |