Increasing trend of northeast monsoon rainfall over the equatorial Indian Ocean and peninsular India
Peninsular India and Sri Lanka receive major part of their annual rainfall during the northeast monsoon season (October–December). The long-term trend in the northeast monsoon rainfall over the Indian Ocean and peninsular India is examined in the vicinity of global warming scenario using the Global...
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| Veröffentlicht in: | Theoretical and applied climatology 2013-04, Vol.112 (1-2), p.185-191 |
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| creator | Prakash, Satya C., Mahesh Sathiyamoorthy, V. Gairola, R. M. |
| description | Peninsular India and Sri Lanka receive major part of their annual rainfall during the northeast monsoon season (October–December). The long-term trend in the northeast monsoon rainfall over the Indian Ocean and peninsular India is examined in the vicinity of global warming scenario using the Global Precipitation Climatology Project (GPCP) dataset available for the period 1979–2010. The result shows a significant increasing trend in rainfall rate of about 0.5 mm day
−1
decade
−1
over a large region bounded by 10 °S–10 °N and 55 °E–100 °E. The interannual variability of seasonal rainfall rate over peninsular India using conventional rain gauge data is also investigated in conjunction to the Indian Ocean dipole. The homogeneous rain gauge data developed by Indian Institute of Tropical Meteorology over peninsular India also exhibit the considerable upward rainfall trend of about 0.4 mm day
−1
decade
−1
during this period. The associated outgoing longwave radiation shows coherent decrease in the order of 2 W m
−2
decade
−1
over the rainfall increase region. |
| doi_str_mv | 10.1007/s00704-012-0719-6 |
| format | Article |
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−1
decade
−1
over a large region bounded by 10 °S–10 °N and 55 °E–100 °E. The interannual variability of seasonal rainfall rate over peninsular India using conventional rain gauge data is also investigated in conjunction to the Indian Ocean dipole. The homogeneous rain gauge data developed by Indian Institute of Tropical Meteorology over peninsular India also exhibit the considerable upward rainfall trend of about 0.4 mm day
−1
decade
−1
during this period. The associated outgoing longwave radiation shows coherent decrease in the order of 2 W m
−2
decade
−1
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−1
decade
−1
over a large region bounded by 10 °S–10 °N and 55 °E–100 °E. The interannual variability of seasonal rainfall rate over peninsular India using conventional rain gauge data is also investigated in conjunction to the Indian Ocean dipole. The homogeneous rain gauge data developed by Indian Institute of Tropical Meteorology over peninsular India also exhibit the considerable upward rainfall trend of about 0.4 mm day
−1
decade
−1
during this period. The associated outgoing longwave radiation shows coherent decrease in the order of 2 W m
−2
decade
−1
over the rainfall increase region.</description><subject>Aquatic Pollution</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric Sciences</subject><subject>Climate change</subject><subject>Climatology</subject><subject>Climatology. Bioclimatology. 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M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Increasing trend of northeast monsoon rainfall over the equatorial Indian Ocean and peninsular India</atitle><jtitle>Theoretical and applied climatology</jtitle><stitle>Theor Appl Climatol</stitle><date>2013-04-01</date><risdate>2013</risdate><volume>112</volume><issue>1-2</issue><spage>185</spage><epage>191</epage><pages>185-191</pages><issn>0177-798X</issn><eissn>1434-4483</eissn><abstract>Peninsular India and Sri Lanka receive major part of their annual rainfall during the northeast monsoon season (October–December). The long-term trend in the northeast monsoon rainfall over the Indian Ocean and peninsular India is examined in the vicinity of global warming scenario using the Global Precipitation Climatology Project (GPCP) dataset available for the period 1979–2010. The result shows a significant increasing trend in rainfall rate of about 0.5 mm day
−1
decade
−1
over a large region bounded by 10 °S–10 °N and 55 °E–100 °E. The interannual variability of seasonal rainfall rate over peninsular India using conventional rain gauge data is also investigated in conjunction to the Indian Ocean dipole. The homogeneous rain gauge data developed by Indian Institute of Tropical Meteorology over peninsular India also exhibit the considerable upward rainfall trend of about 0.4 mm day
−1
decade
−1
during this period. The associated outgoing longwave radiation shows coherent decrease in the order of 2 W m
−2
decade
−1
over the rainfall increase region.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00704-012-0719-6</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0177-798X |
| ispartof | Theoretical and applied climatology, 2013-04, Vol.112 (1-2), p.185-191 |
| issn | 0177-798X 1434-4483 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1323811713 |
| source | Springer Nature - Complete Springer Journals |
| subjects | Aquatic Pollution Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric Sciences Climate change Climatology Climatology. Bioclimatology. Climate change Earth and Environmental Science Earth Sciences Earth, ocean, space Exact sciences and technology External geophysics Global temperature changes Global warming Marine Meteorology Monsoons Nuclear radiation Ocean Oceans Original Paper Rain and rainfall Rain gauges Rainfall measurement Rainfall rate Tidal waves Tropical meteorology Waste Water Technology Water in the atmosphere (humidity, clouds, evaporation, precipitation) Water Management Water Pollution Control |
| title | Increasing trend of northeast monsoon rainfall over the equatorial Indian Ocean and peninsular India |
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