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of 104
pro vyhledávání: '"B. Abish"'
Autor:
Athira P. Ratnakaran, B. Abish
Publikováno v:
Theoretical and Applied Climatology.
Autor:
B. Abish, K. Mohanakumar
Publikováno v:
Annales Geophysicae, Vol 29, Pp 1605-1612 (2011)
The influence of aerosols on cloud properties over North India which includes the Indo-Gangetic Plain has been investigated for the years 2000 to 2010. During the years 2004, 2009 and 2010 there has been an abrupt increase in fine mode aerosol opt
Externí odkaz:
https://doaj.org/article/88a0bb2f68ef44c1ab6fe0f65e4ae411
Akademický článek
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Publikováno v:
Atmospheric Research. 227:125-139
In this study, the weakening of the orographic rainfall for the period 2000–2011 during the Indian summer monsoon (JJA) is investigated using the regional climate model RegCM 4.5. Analysis reveals that when sulfate aerosol feedback is included in t
Publikováno v:
International Journal of Climatology. 38:203-214
The recent Indian Ocean (IO) warming and its relation with the El Nino Southern Oscillation (ENSO) is investigated using available ocean and atmospheric reanalyses. By comparing the events before and after 1976 (identified as a threshold separating e
Publikováno v:
2019 URSI Asia-Pacific Radio Science Conference (AP-RASC).
In this study, the weakening of the Indian summer monsoon circulation is analyzed using the regional climate model RegCM 4.5. It is seen that the when sulfate aerosol component is included in the model run, the simulated temperature shows a cooling a
Autor:
B. Abish, Swadhin K. Behera, P. V. Joseph, Simona Masina, Satyaban B. Ratna, Annalisa Cherchi
Publikováno v:
Climate Dynamics. 46:949-965
The Indo-Pacific Ocean (i.e. region between 30°E and 150°E) has been experiencing a warming since the 1950s. At the same time, the large-scale summer monsoon rainfall over India and the moisture over the East Africa/Arabian Sea are both decreasing.
Publikováno v:
Advances in Atmospheric Sciences. 32:140-148
A study of six decades (1950–2009) of reanalysis data reveals that the subtropical jetstream (STJ) of the Southern (Northern) Hemisphere between longitudes 0 ◦ E and 180 ◦ E has weakened (strengthened) during both the boreal winter (January, Fe
Akademický článek
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Publikováno v:
Journal of Climate. 26:9408-9414
Recent research has reported that the tropical easterly jet stream (TEJ) of the boreal summer monsoon season is weakening. The analysis herein using 60 yr (1950–2009) of data reveals that this weakening of the TEJ is due to the decreasing trend in