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, or bare ground) or broader deforestation regions (not confined to the tropics). Besides impacting local and regional climate, large-scale deforestations can also induce remote climate impacts through changes in the large-scale circulation (e.g., Hadley circulation or Walker circulation) and Rossby wave propagation in the atmosphere (e.g., Henderson-Sellers et al. 1993 ; Sud et al. 1996 ; Zhang et al. 1996b ; Snyder 2010 ; Lawrence and Vandecar 2015 ). Mesoscale deforestation (on scales of
, or bare ground) or broader deforestation regions (not confined to the tropics). Besides impacting local and regional climate, large-scale deforestations can also induce remote climate impacts through changes in the large-scale circulation (e.g., Hadley circulation or Walker circulation) and Rossby wave propagation in the atmosphere (e.g., Henderson-Sellers et al. 1993 ; Sud et al. 1996 ; Zhang et al. 1996b ; Snyder 2010 ; Lawrence and Vandecar 2015 ). Mesoscale deforestation (on scales of
