| Summary: | The Greenland Ice Sheet covers over 80% of Greenland’s land area and is the largest reservoir of frozen water in the Northern Hemisphere. Over the past few decades, the Greenland Ice Sheet has experienced significant summertime ice and surface snow loss. Much of this mass loss can be attributed to short-term processes that initiate surface energy changes. In this dissertation, we examine the effects of 1) light-absorbing aerosols on the Greenland Ice Sheet and in the overlying atmosphere, 2) the impacts of atmospheric block location over the Greenland Ice Sheet on cloud formation and atmosphere-surface energy exchanges, and 3) how these block-induced surface energy responses will change in the future. Aerosols are microscopic solid or liquid particles that can be transported long distances through the atmosphere. Light-absorbing aerosols like black carbon and certain types of dust are unique in that they absorb sunlight and warm the local environment. In the Arctic, black carbon reduces surface reflectivity and increases surface energy to induce or enhance melt. Light- absorbing aerosols suspended in the atmosphere warm the local air and change vertical circulation patterns. We use an idealized version of the Community Earth System Model (CESM) to understand how Greenland-specific local atmospheric and in-snow light-absorbing aerosols can affect Greenland Ice Sheet surface energy input and snowmelt processes. Overall, we find that the largest snowmelt and net surface energy responses occur in simulations containing only in-snow light-absorbing aerosols while atmospheric absorbing aerosols decrease incident sunlight on the surface and produce insignificant melt and energy changes. Atmospheric and in-snow aerosols have offsetting effects on the surface energy budget. Atmospheric blocks are mostly stationary high pressure systems that last for days to weeks at a time. Blocking over Greenland has been shown to enhance net surface energy by reducing cloud cover and transporting warm, moist air over the surface. The ...
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