Thunder-storms began to develop late afternoon early evening along a well defined dry-line in the eastern sector of the Permian Basin, along the southern said boundary, associated with an intense Upper Level Low centered in the central Rockies. The Upper Level Low and associated short wave troughs broke down an entrenched Upper-mid Level High which had controlled the weather across the Permian Basin for several days with above normal temperatures, exceeding the century mark. Low level moisture was present early in the morning and early afternoon hours, extending into the central Permian Basin but was gradually displaced eastward by strong westerly winds mixing downward from the base of the Upper Level Low, advancing from the western US. At 2000Z the author drove to Big Spring awaiting dry-line initiation where cumulus clouds had developed along the dry-line but mid level capping inversion was still in place preventing storm tower growth. The first image is a screen capture from the truck at previously mentioned locale depicting surface winds and defining dry-line with intersection of same and SPC depicting thunderstorm probability east of Midland. After watching the dry-line locale with cumulus cloud development for one hour, with no storm tower development, the author had to return to Midland. Later in the evening storm tower and organized cell development occurred. The next image was taken at 0115Z in a parking lot in Midland looking east-northeast at dry-line induced convection.
Thursday, June 5, 2008
Dry-Line Thunderstorms, Eastern Permian Basin, June 5th, 2008
Thunder-storms began to develop late afternoon early evening along a well defined dry-line in the eastern sector of the Permian Basin, along the southern said boundary, associated with an intense Upper Level Low centered in the central Rockies. The Upper Level Low and associated short wave troughs broke down an entrenched Upper-mid Level High which had controlled the weather across the Permian Basin for several days with above normal temperatures, exceeding the century mark. Low level moisture was present early in the morning and early afternoon hours, extending into the central Permian Basin but was gradually displaced eastward by strong westerly winds mixing downward from the base of the Upper Level Low, advancing from the western US. At 2000Z the author drove to Big Spring awaiting dry-line initiation where cumulus clouds had developed along the dry-line but mid level capping inversion was still in place preventing storm tower growth. The first image is a screen capture from the truck at previously mentioned locale depicting surface winds and defining dry-line with intersection of same and SPC depicting thunderstorm probability east of Midland. After watching the dry-line locale with cumulus cloud development for one hour, with no storm tower development, the author had to return to Midland. Later in the evening storm tower and organized cell development occurred. The next image was taken at 0115Z in a parking lot in Midland looking east-northeast at dry-line induced convection.
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