Contribution of Atmospheric Advection to the Amplified Winter Warming in the Arctic North Atlantic Region. (20th November 2017)

• Record Type: Journal Article
• Authors: Dahlke, Sandro; Maturilli, Marion
• Other Names: Cherchi Annalisa Academic Editor.
• Is Part Of: Advances in meteorology. Volume 2017(2017)
• Publication Date: 2017-11-20
• Subjects: Meteorology -- Periodicals; Meteorology; Periodicals; 551.505
• DOI: 10.1155/2017/4928620
• Languages: English
• ISSNs: 1687-9309

Abstract

Abstract : Arctic Amplification of climate warming is caused by various feedback processes in the atmosphere-ocean-ice system and yields the strongest temperature increase during winter in the Arctic North Atlantic region. In our study, we attempt to quantify the advective contribution to the observed atmospheric warming in the Svalbard area. Based on radiosonde measurements from Ny-Ålesund, a strong dependence of the tropospheric temperature on the synoptic flow direction is revealed. Using FLEXTRA backward trajectories, an increase of advection from the lower latitude Atlantic region towards Ny-Ålesund is found that is attributed to a change in atmospheric circulation patterns. We find that about one-quarter (0.45 K per decade) of the observed atmospheric winter near surface warming trend in the North Atlantic region of the Arctic (2 K per decade) is due to increased advection of warm and moist air from the lower latitude Atlantic region, affecting the entire troposphere.