Meteorological Analysis
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TD 22 originated from a mid/upper level low which formed over the Atlantic on the 5th. A
surface trough formed in association with the low on October 6th. The surface trough
became closed on October 8th as convection increased, and a subtropical depression
formed. It was about 500 nm from Bermuda at the time. As the depression turned west
on the north side of the low on the 9th, shear intensified. By the 10th the depression was a
remnant low, drifting about 150 nm from Bermuda. The low turned northwestward and
joined with a cold front off of Cape Hatteras on the 11th. It became an extra-tropical gale
on this front and affected the Mid-Atlantic until the 14th. The low was absorbed on the 14th.
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Casualty and Damage Overview
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There were no reports of damage or casualties in association with TD 22.
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Imagery
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Tracking Data
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Subtropical Depression Twenty-Two (8-9 October 2005)
Track positions and wind speeds:
INITIAL 08/1500Z 28.1N 59.0W 30 KT
INITIAL 08/2100Z 29.1N 60.8W 30 KT
INITIAL 09/0300Z 29.2N 62.6W 25 KT...DISSIPATING
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Tracking map courtesy of Plymouth
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Selected Satellite Image
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