The deep subtropical trough that I mentioned in
yesterday's post is responsible for the powerful storms in the Caribbean that are the likely cause of a
plane crash in Kingston, Jamaica last night. The crash occurred at 322Z (10:22PM local time) in heavy rain and with a ceiling of 1,400 feet (details
here). The following satellite images are from 315Z and 345Z (7 minutes before and 23 minutes after the crash).
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Water vapor images for the same times:
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Although the heaviest storms and coldest cloudtops do not appear to be over the
exact location of the crash, there are some storms backbuilding across southeast Jamaica between 3 and 4Z. This can be seen more easily in color enhanced images:
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Close-up of 3Z:
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Close-up of 4Z:
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Rain was not reported at the airport until 1Z, and heavy rain not until 3Z. Wind was from the northwest at 8 knots at 3Z, but increased to 14 by 4Z. Even more telling, visibility was 5 km at 228Z, 3 km at 300Z, and 1.5 km by400Z. It is easy to see how a crash could have occurred under such rapidly deteriorating conditions. Here is the last useful visible image from yesterday.
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This is all a result of a large upper trough extending down into Central America.
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A surface trough of 1008 mb develops about 100 miles southeast of Jamaica by 6Z.
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Meanwhile, another incredible storm has almost all of the Plains and upper Mississippi Valley under a winter storm warning (pink), areas near Chicago an ice storm warning (purple), and the deep south under tornado watches and warnings (yellow and red), and it is only getting started.
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And Europe also continues to get almost nonstop brutal winter weather including temperatures to -20C in Poland, -33C in Germany, crippling snowstorms in Moscow, and unusual heavy snow in Milan, Italy. See more
here.
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