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Windstorm Review

Late Winter Squall Line. GOES Microburst Windspeed Potential Index (. MWPI) product performed effectively during a late winter squall line event that occurred on 28 February 2011. During the morning of 28 February, an intense squall line developed ahead of a cold front over the Appalachian Mountains and tracked through Virginia, eastern West Virginia, and central Maryland. Downburst wind gusts of 37 to 38 knots were recorded by RWIS sensors over western Frederick County, Maryland between 1500 and 1530 UTC.

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Late Winter Squall Line. GOES Microburst Windspeed Potential Index (. MWPI) product performed effectively during a late winter squall line event that occurred on 28 February 2011. During the morning of 28 February, an intense squall line developed ahead of a cold front over the Appalachian Mountains and tracked through Virginia, eastern West Virginia, and central Maryland. Downburst wind gusts of 37 to 38 knots were recorded by RWIS sensors over western Frederick County, Maryland between 1500 and 1530 UTC.

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Windstorm Review | windstormreview.blogspot.com Reviews

https://windstormreview.blogspot.com

Late Winter Squall Line. GOES Microburst Windspeed Potential Index (. MWPI) product performed effectively during a late winter squall line event that occurred on 28 February 2011. During the morning of 28 February, an intense squall line developed ahead of a cold front over the Appalachian Mountains and tracked through Virginia, eastern West Virginia, and central Maryland. Downburst wind gusts of 37 to 38 knots were recorded by RWIS sensors over western Frederick County, Maryland between 1500 and 1530 UTC.

INTERNAL PAGES

windstormreview.blogspot.com

1

Windstorm Review: May 2010

http://windstormreview.blogspot.com/2010_05_01_archive.html

Oklahoma Tornadoes and Downbursts. Figure 1. Surface analysis of Oklahoma Mesonet observations at 2000 UTC (top) and GOES MWPI product at 1919 UTC (bottom). Figure 2. RAOB from Norman, OK at 2000 UTC. Figure 3. GOES MWPI product at 2121 UTC and BTD image product at 2215 UTC with overlying radar reflectivity image from Oklahoma City TDWR. Severe weather occurred in the Norman area with the following time line:. 2218-Tornado touches down near Moore associated with supercell #1. Links to this post.

2

Windstorm Review: October 2010

http://windstormreview.blogspot.com/2010_10_01_archive.html

Revised Virtual Institute for Satellite Integration Training (VISIT) Lesson. Institute for Satellite Integration Training (VISIT) Lesson titled “. Nvective Downburst Potential Using GOES Sounder Derived Products. 8221; has been revised by K. Pryor to include new case studies and new instructional material pertaining to the Graphyte Toolkit and the Geostationary Operational Environmental Satellite (GOES) channel 3 – channel 4 brightness temperature difference (BTD) product. Links to this post. Recent deve...

3

Windstorm Review: November 2010

http://windstormreview.blogspot.com/2010_11_01_archive.html

Strong November Storms over Mid-Atlantic Region. Figure 1. GOES-13 WV-IR BTD image at 0615 UTC with overlying radar reflectivity from Sterling, VA NEXRAD. Figure 2. GOES-13 WV-IR BTD image at 0615 UTC with overlying radar velocity from Sterling, Virginia NEXRAD. The Tidal Potomac Region was also effected by the squall line between 0545 and 0630 UTC, as evidenced by high winds recorded by NOAA data buoys and WeatherFlow. Figure 6. GOES-13 WV-IR BTD image at 0632 UTC with overlying radar reflectivity f...

4

Windstorm Review: December 2010

http://windstormreview.blogspot.com/2010_12_01_archive.html

December Begins with a Windstorm. Observing stations. Similar to the 17 November downburst event, the channeling of mid-tropospheric dry air into the core of convective storms provided significant downdraft energy that resulted in high winds. Figure 1. GOES-13 VW-IR brightness temperature difference (BTD) image at 1445 UTC 1 December 2010. Figure 2. Radiosonde observation (RAOB) from Dulles Airport, VA at 1200 UTC 1 December 2010. Figure 3. Thomas Point Lighthouse, Maryland. Links to this post.

5

Windstorm Review: December 2009

http://windstormreview.blogspot.com/2009_12_01_archive.html

The March 2004 Chesapeake Bay Downburst Event. Analysis of RUC model data has provided new results from the study of the March 2004 Chesapeake Bay downburst event. This event was associated with the Baltimore water taxi accident that occurred during the afternoon of 6 March 2004, discussed in a previous entry. Figure 1. RUC derived temperature lapse rate,. Vertical humidity difference (dRH, middle), and. Precipitable water (PW, bottom). At 2000 UTC 6 March 2004. With overlying NEXRAD radar reflectivity.

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Windstorm Review

Late Winter Squall Line. GOES Microburst Windspeed Potential Index (. MWPI) product performed effectively during a late winter squall line event that occurred on 28 February 2011. During the morning of 28 February, an intense squall line developed ahead of a cold front over the Appalachian Mountains and tracked through Virginia, eastern West Virginia, and central Maryland. Downburst wind gusts of 37 to 38 knots were recorded by RWIS sensors over western Frederick County, Maryland between 1500 and 1530 UTC.

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