dennis vs the ridge: major hurricane dynamics
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- weatherwindow
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dennis vs the ridge: major hurricane dynamics
having followed dennis closely(for obvious reasons), i was struck by an apparent contradiction. it was my understanding that the outflow anticyclone of a major hurricane CAN reinforce the synoptic ridge to its poleward side, in effect, reinforceing its steering currents. an earlier post suggested that a major hurricane, as a mesoscale low, CAN assist in eroding that ridging. are both of these effects valid? and can anyone shine additional light on it. this may become very important in the next 72 hours as the ridge strength is crucial for the keys and the fla peninsula......thanks for your comments.........................rich
Last edited by weatherwindow on Wed Jul 06, 2005 4:49 am, edited 1 time in total.
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- weatherwindow
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- TreasureIslandFLGal
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Rich:
This is a great question.
I have my own guesses to answer your questions--
A Hurricane is a low at the surface, but the low reverses itself with height, that means around a major storm (emphasis on Major), the outflow from the upper levels of the cane can reinforce the ridging. Air subsides all around the storm. As it does, it makes sense that it would raise pressures all around the storm. I think we all probably focus on the ridge to poleward because weakening and strengthening of that ridge has everything to do with recurvature or not. So, yes, with a major storm, a hurricane can enhance the ridge. I think it has to be big & strong, though. A hurricane is smaller scale than the ridges that drive it. It would take a lot of air to affect them.
Your second question--about why sometimes we say a hurricane leaves a wake like a mesoscale low--is an interesting one. While I am not sure of the answer...I wonder if it has the fact to do that we say this mainly when we are looking at situations where a hurricane has gone around the periphery of a ridge (beginning or in a poleward turn already). In other words, a hurricane goes to a weakness or erosion in a ridge (often caused/in conjunction with a 500 MB trough) during poleward curvature. So upper levels are already a little lower pressure (and height) where the hurricane is than in the nearby ridge. The recurving hurricane, with its low pressure, is going to make the "weakened" ridge even weaker in the short term. And that can linger after the storm passes.
Educated guesses. I leave it to the professional mets to correct, enhance, etc.
Great questions.
This is a great question.
I have my own guesses to answer your questions--
A Hurricane is a low at the surface, but the low reverses itself with height, that means around a major storm (emphasis on Major), the outflow from the upper levels of the cane can reinforce the ridging. Air subsides all around the storm. As it does, it makes sense that it would raise pressures all around the storm. I think we all probably focus on the ridge to poleward because weakening and strengthening of that ridge has everything to do with recurvature or not. So, yes, with a major storm, a hurricane can enhance the ridge. I think it has to be big & strong, though. A hurricane is smaller scale than the ridges that drive it. It would take a lot of air to affect them.
Your second question--about why sometimes we say a hurricane leaves a wake like a mesoscale low--is an interesting one. While I am not sure of the answer...I wonder if it has the fact to do that we say this mainly when we are looking at situations where a hurricane has gone around the periphery of a ridge (beginning or in a poleward turn already). In other words, a hurricane goes to a weakness or erosion in a ridge (often caused/in conjunction with a 500 MB trough) during poleward curvature. So upper levels are already a little lower pressure (and height) where the hurricane is than in the nearby ridge. The recurving hurricane, with its low pressure, is going to make the "weakened" ridge even weaker in the short term. And that can linger after the storm passes.
Educated guesses. I leave it to the professional mets to correct, enhance, etc.
Great questions.
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pavelbure224
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- weatherwindow
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I think the ridge will be stronger than many are prediciting. It appears that Cindy may be pumping the Ridge to the north. If you look at the latest Water Vapor, notice the southwestern movement of the High (Anticyclonic circulation) centered over NE FL. Secondly, I noticed how the clouds in the most northern band of Dennis are flattening out.
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