Above 500 mbs, the environment is hostile and according to the 12z run, model data above 500 will be even more hostile, as a full latitude trough sets up shop on the east coast. The upper low to the west of the LLC is forecasted to dissipate as it moves west . As for the convection to the east, I expect to see this evolve into a dynamic low with frontogenesis as trough deepens along the coast and ridge shifts westward and builds with approaching EPAC system. As a shallow system, Alberto will be in a COL between mid-continental ridge and Atlantic ridge and above EC longwave trough to it's northeast and left to dissipate in GOM
"Survived Trigonometry and Calculus I"
Edited by AlaberryPatch (Sun Jun 11 2006 02:21 PM)
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