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Titel |
Association of the pre-monsoon thermal field over north India and the western Tibetan Plateau with summer monsoon rainfall over India |
VerfasserIn |
S. D. Bansod, S. Fadnavis, S. P. Ghanekar |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
0992-7689
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Digitales Dokument |
URL |
Erschienen |
In: Annales Geophysicae ; 33, no. 8 ; Nr. 33, no. 8 (2015-08-25), S.1051-1058 |
Datensatznummer |
250121239
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Publikation (Nr.) |
copernicus.org/angeo-33-1051-2015.pdf |
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Zusammenfassung |
In this paper, interannual variability of tropospheric air temperatures over
the Asian summer monsoon region during the pre-monsoon months is examined in
relation to Indian summer monsoon rainfall (ISMR; June to September total
rainfall). For this purpose, monthly grid-point temperatures in the entire
troposphere over the Asian summer monsoon region and ISMR data for the period
1949–2012 have been used. Spatial correlation patterns are investigated
between the temperature field in the lower tropospheric levels during May
over the Asian summer monsoon region and ISMR. The results indicate a strong
and significant northwest–southeast dipole structure in the spatial
correlations over the Indian region, with highly significant positive
(negative) correlations over the regions of north India and the western
Tibetan Plateau region – region R1 (north Bay of Bengal: region R2). The
observed dipole is seen significantly up to a level of 850 hPa and
eventually disappears at 700 hPa. Thermal indices evaluated at 850 hPa
level, based on average air temperatures over the north India and western
Tibetan Plateau region (TI1) and the north Bay of Bengal region
(TI2) during May, show a strong, significant relationship with the ISMR.
The results are found to be consistent and robust, especially in the case of
TI1 during the period of analysis. A physical mechanism for the
relationship between these indices and ISMR is proposed. Finally the
composite annual cycle of tropospheric air temperature over R1 during
flood/drought years of ISMR is examined. The study brings out the importance
of the TI1 in the prediction of flood/drought conditions over the Indian
subcontinent. |
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