Globally the marine environment has been undergoing rapid change due to anthropogenic activities (Field et al., 2014;Gattuso et al., 2018). This is especially true for the high-latitude oceans, where warming is occurring faster than the rest of the world (Blunden & Arndt, 2016;Neukermans et al., 2018). In the Pacific Arctic, changing environmental conditions have been documented in the area where the North Pacific meets the Arctic Ocean encompassing the Bering, Beaufort, and Chukchi Seas, including dramatic reductions in sea ice extent (Grebmeier et al., 2010), shifts in biological communities (Brodeur et al., 2008;Will et al., 2020), changes in patterns of primary production (Arrigo & van Dijken, 2015), and alterations in species phenology (e.g., timing of phytoplankton blooms, ice dynamics, and species migrations and reproduction; Hill et al., 2018;Moore, 2016). How species will fare in the Pacific Arctic during this