“…Irrespective of whether lake coverage is expanding or decreasing, the reorganization of thermokarst lake cover will have significant implications for polar atmospheric carbon fluxes (Engram et al., 2020; Grosse et al., 2013; Petrescu et al., 2010; Rowland et al., 2010; van Huissteden et al., 2011; Walter Anthony et al., 2018). Moreover, thermokarst lakes in deltas modulate the transport of riverine freshwater, sediment, and nutrient fluxes to the Arctic ocean, by trapping and holding sediment (Marsh et al., 1999; Piliouras & Rowland, 2020) and modifying the residence times and pathways of nutrient transport through the delta (Cunada et al., 2021; Emmerton et al., 2007; Lesack & Marsh, 2010; Squires et al., 2009; Tank et al., 2009). Therefore, changing deltaic lake coverage and its spatial distribution will also alter the timing and magnitudes of riverine fluxes to the Arctic Ocean, which has broader implications for near‐shore circulation and ecosystem productivity (Lique et al., 2016).…”