A large and growing body of research suggests that the magnitude of warming due to anthropogenic climate change in the Arctic is four times the global average (Previdi et al., 2021;Rantanen et al., 2022;Serreze & Barry, 2011). This Arctic amplification is partly due to sea ice loss across the Arctic, which decreases regional albedo and amplifies warming, a process known as the sea ice-albedo feedback (Hudson, 2011;Perovich & Polashenski, 2012;Previdi et al., 2021; Winton, 2006). The extreme magnitude of this warming drives ongoing shifts in Arctic vegetation, with shrubs and trees increasing cover in areas previously consisting of graminoid
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