Cape Farewell, Greenland's southernmost point, is a region of significant interest in the meteorological and oceanographic communities in that atmospheric flow distortion associated with the high topography of the region leads to a number of high wind speed jets. The resulting large air-sea fluxes of momentum and buoyancy have a dramatic impact on the region's weather and ocean circulation. Here the first in-situ observations of the surface meteorology in the region, collected from an instrumented buoy, are presented. The buoy wind speeds are compared to 10 m wind speeds from the QuikSCAT satellite and the North American Regional Reanalysis (NARR). We show that the QuikSCAT retrievals have a high wind speed bias that is absent from the NARR winds. The spatial characteristics of the high wind speed events are also presented. Copyright 2008 by the American Geophysical Union.
CITATION STYLE
Moore, G. W. K., Pickart, R. S., & Renfrew, I. A. (2008). Buoy observations from the windiest location in the world ocean, Cape Farewell, Greenland. Geophysical Research Letters, 35(18). https://doi.org/10.1029/2008GL034845
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