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• W2076323570 endingPage "17468" @default.
• W2076323570 startingPage "17468" @default.
• W2076323570 abstract "The high ice-covered topography of Greenland represents a significant barrier to atmospheric flow and, as a direct and indirect result, it plays a crucial role in the coupled climate system. The wind field over Greenland is important in diagnosing regional weather and climate, thereby providing information on the mass balance of the ice sheet as well as assisting in the interpretation of ice core data. Here, we identify a number of hitherto unrecognised features of the three-dimensional wind field over Greenland; including a 2500-km-long jet along the central ice sheet’s western margin that extends from the surface into the middle-troposphere, as well as a similar but smaller scale and less intense feature along its eastern margin. We refer to these features as Greenland Plateau Jets. The jets are coupled to the downslope katabatic flow and we argue that they are maintained by the zonal temperature gradients associated with the strong temperature inversion over the central ice sheet. Their importance for Greenland's regional climate is discussed." @default.
• W2076323570 created "2016-06-24" @default.
• W2076323570 creator A5010704341 @default.
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• W2076323570 date "2013-12-01" @default.
• W2076323570 modified "2023-09-24" @default.
• W2076323570 title "Greenland plateau jets" @default.
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• W2076323570 doi "https://doi.org/10.3402/tellusa.v65i0.17468" @default.
• W2076323570 hasPublicationYear "2013" @default.
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