Resolving the Weakening of Orographic Rainfall Over India Using a Regional T Climate Model Regcm 4.5 ⁎ B
1 Atmospheric Research 227 (2019) 125–139 Contents lists available at ScienceDirect Atmospheric Research journal homepage: www.elsevier.com/locate/atmosres Resolving the weakening of orographic rainfall over India using a regional T climate model RegCM 4.5 ⁎ B. Abisha,c, , K. Aruna,b a Nansen Environmental Research Centre India, Kochi, India b Department of Atmospheric Sciences, Cochin University of Science and Technology, Kochi, India c Kerala University of Fisheries and Ocean Studies, Kochi, India ARTICLE INFO ABSTRACT Keywords: In this study, the weakening of the orographic rainfall for the period 2000–2011 during the Indian summer RegCM 4.5 monsoon (JJA) is investigated using the regional climate model RegCM 4.5. Analysis reveals that when sulfate Orographic rainfall aerosol feedback is included in the model run, the simulated temperature shows a cooling of the continental Indian summer monsoon upper troposphere by 0.3 °C. At the same time, the sulfate aerosol loading in the atmosphere had induced cooling Climate change of 0.2 °C of the lower troposphere over the Indian region. Consequently, the simulated zonal wind fields show a Sulfate aerosols weakening at the upper and lower tropospheric levels, particularly where the semi-permanent systems that drive the monsoon circulations are located. It is suggested that the weakening of zonal winds has caused a suppression of the orographic rainfall along the west coast of India (Western Ghats), as evident from the observations. Concurrently, the simulations indicate a sulfate aerosol induced reduction in orographic monsoon rainfall over the southern Western Ghats, whereas their effect is insignificant in controlling the orographic rainfall inthe northern Western Ghats.
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