#31 Postby frederic79 » Tue Jul 26, 2005 9:11 am
There was a comment recently in an advisory on Emily...
WHILE WE OFTEN TALK ABOUT THE COLD WAKE THAT HURRICANES LEAVE
BEHIND...IT APPEARS THAT HURRICANE DENNIS HAS ACTUALLY MADE
PORTIONS OF THE CARIBBEAN SEA WARMER...AND HENCE MORE FAVORABLE FOR THE POTENTIAL DEVELOPMENT OF EMILY. HEAT CONTENT ANALYSES FROM THE UNIVERSITY OF MIAMI INDICATE THAT WESTERLY WINDS ON THE SOUTH SIDE OF DENNIS HAVE SPREAD WARM WATERS FROM THE NORTHWESTERN CARIBBEAN EASTWARD TO THE SOUTH AND SOUTHEAST OF JAMAICA...AN AREA THAT COULD BE TRAVERSED BY EMILY IN THREE DAYS OR SO.
FORECASTER FRANKLIN
My question is this: Although typically buoy SST's represent oceanic heat content to a limited depth in the Gulf as Derek mentioned, could upwelling from two Catagory 4 hurricanes in July (unprecedented) cause the warmer surface layer to mix with the colder water down deep and eventually caused greater oceanic heat content in the affected areas?
Okay, back to the swimming pool (seriously). If I reach down to check the chlorine in water that has been sitting untouched, the top layer is warmer than the bottom layer. But if the kids have been swimming and mixing it up, it all feels like the same temperature, albeit slightly cooler.In the Gulf, we know 82 degrees F or so is sufficient in sustaining a major hurricane, so upwelling doesn't necessarily cool the water enough to prohibit this when the temps remain in the 80's at the surface. Simulaneously deeper, colder water is pulled to the surface and eventually warmed as warmer surface water goes deeper.
Does this idea hold water (pun intended)?
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