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Gulf of Alaska Noreaster
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If lows and highs aloft and at the surface are above one another, the systems will weaken !
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Divergence aloft promotes the surface low Convergence aloft promotes the surface high Surface divergence Surface convergence
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Longwaves
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MIGRATE THROUGH THE LONGWAVE TROUGHS Chapter 10, page 312 Aguado & Burt
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1 2 3 Differential temperature advection intensifies the wave Condensation may release even more heat energy for the storm Less upper level divergence No temp advection
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