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The response of low-latitude weather and climate to polar sea ice melt is not well understood. In this study, we run a suite of coupled and uncoupled simulations using the Community Earth System Model to investigate the effects of polar sea ice melt on western disturbance (WD) activity over the Indian subcontinent. In the coupled model simulation, the albedo of the sea ice is reduced in such a way that the increased absorption of the solar radiation would melt the sea ice. Further, the monthlydoi:10.21203/rs.3.rs-2132087/v1 fatcat:x35rukq35zejzay44ppunxtkhm