A New Look at the Summer Arctic Frontal Zone

• Published in: Journal of climate 2015-01, Vol.28 (2), p.737-754
• Main Authors: Crawford, Alex, Serreze, Mark
• Format: Article
• Language: English
• Subjects: Accuracy; Algorithms; Annual variations; Arctic fronts; Arctic zone; Atmosphere; Atmospheric heating; Cloud cover; Coastal waters; Coasts; Cyclones; Ecosystems; Energy balance; Heating; Ice; Interannual variations; Land; Land surface temperature; Ocean temperature; Oceans; Precipitation; Sea ice; Sea level; Snow; Snow cover; Studies; Summer; Surface energy; Surface energy balance; Surface properties; Surface wind; Taiga & tundra; Temperature; Temperature dependence; Temperature gradients; Timberlines; Troposphere; Variability; Vegetation; Wind; Wind direction
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-14-00447.1

A notable characteristic of the summertime Arctic is the existence of a narrow band of strong horizontal temperature gradients spanning the coastlines of Siberia, Alaska, and western Canada that extends through a considerable depth of the troposphere. Past research has associated this summer Arctic Frontal Zone (AFZ) with contrasts in atmospheric heating between the Arctic Ocean and snow-free land, with its regional strength strongly influenced by topography; however, little is known about its variability. In this study, output from the latest generation of global atmospheric reanalyses is used to better constrain and define the summer AFZ, including its spatial and seasonal characteristics. The relative importance of different factors linked to its variability is then evaluated. The AFZ is best expressed in July and is manifested aloft as a separate Arctic jet feature at about 250 hPa. It is clearly associated with differential atmospheric heating, as evidenced by the sharp difference in surface energy balance terms between the Arctic Ocean and land. Furthermore, the AFZ is strongest over the coastline whether observed near the surface or throughout the troposphere. Interannual variations in peak strength of the AFZ are spatially heterogeneous and systematic near the surface (the 2-m level). Spatiotemporal variability is primarily dependent on factors affecting temperature over land, especially variability in cloud cover, surface wind direction, and the timing of the annual snow cover retreat. Local variability in the timing of annual sea ice retreat is also important through its control on temperatures over coastal seas.