Abstract
The previous decade and a half saw major advances in understanding of the Arctic atmosphere and the ability to project future climate states based on reanalysis datasets, field studies, and climate models. Limitations continue to be the lack of direct observations of the Arctic troposphere. The balance of evidence now argues for an anthropogenic component to Arctic change. Today, we see positive Arctic-wide temperature trends in all seasons with an Arctic amplification relative to lower latitude changes, but with strong regional modulations from natural variability. These include a positive index of the Arctic Oscillation (AO) in the early 1990s, a record negative phase of the AO during the winter of 2009/2010, and increased prominence of an Arctic Dipole (AD) climate pattern. The negative AO period showed linkages between Arctic and subarctic weather. Despite deficiencies in climate models used for the International Panel of Climate Change (IPCC), all models project increased temperatures and sea ice loss by mid-century, amplified through Arctic feedback processes.
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Overland, J.E., Serreze, M.C. (2012). Advances in Arctic Atmospheric Research. In: Lemke, P., Jacobi, HW. (eds) Arctic Climate Change. Atmospheric and Oceanographic Sciences Library, vol 43. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-2027-5_2
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