Frances Being Stationery Has Helped
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- Sean in New Orleans
- Category 5

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Frances Being Stationery Has Helped
It's a good thing that Frances has been stationery for the last day..it has helped the storm to weaken as the system has churned deep cooler waters to the surface which is weakening the system before our eyes. This is a real blessing to see this storm weaken. Frances could strengthen, though, just before reaching West Central Florida when the system moves over warmer waters...
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Re: Frances Being Stationery Has Helped
Sean in New Orleans wrote:It's a good thing that Frances has been stationery for the last day..it has helped the storm to weaken as the system has churned deep cooler waters to the surface which is weakening the system before our eyes. This is a real blessing to see this storm weaken. Frances could strengthen, though, just before reaching West Central Florida when the system moves over warmer waters...
you may be right but an earlier post stated the upwelling is not an issue here. If I remember right it would have to sit in one place for 48 hours. But what do I know Im a new guy here..lol...
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frankthetank
- Category 2

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heres an overlay from this afternoon
high res http://rapidfire.sci.gsfc.nasa.gov/gall ... 4.250m.jpg
high res http://rapidfire.sci.gsfc.nasa.gov/gall ... 4.250m.jpg
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- opera ghost
- Category 4

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- Location: Houston, Texas
Here's a link to the bathymetry.
http://walrus.wr.usgs.gov/infobank/gaze ... y/bhs.html
They are shallow indeed. More important than bathymetry is the depth of the mixed layer of the ocean because that controls how much heat the upper ocean contains and how quickly mixing/upwelling cools the SSTs. I don't believe the shallowness of the water around the Bahamas are the problem. The main problem is still with the upper atmospheric winds and perhaps some dry air intrusion around 500mb.
http://walrus.wr.usgs.gov/infobank/gaze ... y/bhs.html
They are shallow indeed. More important than bathymetry is the depth of the mixed layer of the ocean because that controls how much heat the upper ocean contains and how quickly mixing/upwelling cools the SSTs. I don't believe the shallowness of the water around the Bahamas are the problem. The main problem is still with the upper atmospheric winds and perhaps some dry air intrusion around 500mb.
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