During the afternoon of
The image above is a Moderate Resolution Imaging Spectroradiometer (MODIS) derived microburst risk product at 1810 UTC 29 March 2009 with overlying radar reflectivity and radial velocity from Sterling, Virginia NEXRAD (KLWX) at 1904 UTC. The microburst product image displays a convective storm line tracking eastward through Frederick County, Maryland into a region of elevated microburst risk (orange shading) with output brightness temperature difference (BTD) values greater than 40K. Based on previous validation of the GOES-11 imager microburst product (Pryor 2009), output BTD greater than 40K is associated with wind gust potential of greater than 40 knots. Radial velocity values, immediately downstream of the storm line, were indicated to be in the 35 to 48 knot range. At this close range to the radar location, radial velocity can serve as a fair estimate of surface winds, and thus, in the absence of measured surface winds, could be used for verification purposes.
References
Pryor, K.L., 2009: Microburst windspeed potential assessment: progress and developments. Preprints, 16th Conf. on Satellite Meteorology and Oceanography, Phoenix, AZ, Amer. Meteor. Soc.
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