Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) (Field Campaign Report)

• Main Authors: Shupe, Matthew, Chu, David, Costa, David, Cox, Christopher, Creamean, Jesse, de Boer, Gijs, Dethloff, Klaus, Engelmann, Ronny, Gallagher, Michael, Hunke, Elizabeth, Maslowski, Wieslaw, McComiskey, Allison, Osborn, Jackson, Persson, Ola, Powers, Heath, Pratt, Kerri, Randall, David, Solomon, Amy, Tjernstrom, Michael, Turner, David, Uin, Janek, Uttal, Taneil, Verlinde, Johannes, Wagner, David
• Language: unknown
• Published: 2021
• Subjects: 54 ENVIRONMENTAL SCIENCES; Arctic; ice pack; Sea ice
• Online Access: http://www.osti.gov/servlets/purl/1787856; https://www.osti.gov/biblio/1787856; https://doi.org/10.2172/1787856

The Arctic is rapidly changing, and these changes have substantial societal relevance. First, arctic change is a leading sign of global change, as the warming observed in the Arctic is 2-3 times faster than observed across the rest of the globe. This so-called arctic amplification is due to numerous feedbacks, including those linked to the declining sea ice. Broad arctic changes are also hypothesized to be related to shifts in large-scale circulation patterns that may have implications for mid-latitude weather and ocean circulation. Arctic change is further affecting the oceans through acidification that threatens food supplies. Declining sea ice also opens the Arctic for new resource development, shipping routes, tourism, and other commercial activities. Lastly, the changing Arctic is a hotbed for geopolitical challenges as nations vie for influence and control of this resource-rich and newly accessible region. Clearly the Arctic and its changes are playing a huge role in our Earth both from a geophysical and socio-political standpoint. To navigate, manage, and respond to the challenges associated with arctic change requires a vastly improved understanding of the coupled arctic system, and the drivers and implications of these changes. It is essential to better understand the physical basis for why the arctic sea ice is declining, the associated feedbacks that work to amplify or modulate this decline, and the myriad ways that the Earth system is responding. As a result of these changes and uncertainties, there are increasing societal needs for improved model predictive skill in the Arctic, to address pressing gaps in global climate prediction, to advance forecast skills for regional and hemispheric weather and sea ice, and to ensure robust ecosystem models that realistically link physical and biological systems. To fulfill these core needs requires new, sophisticated, and cross-cutting observations within the rapidly changing arctic ice pack.