Dr. Jeff Masters' WunderBlog |
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| Posted by: Dr. Jeff Masters, 1:16 PM GMT on April 07, 2006 | +0 |


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Jeff co-founded the Weather Underground in 1995 while working on his Ph.D. He flew with the NOAA Hurricane Hunters from 1986-1990.
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http://www.goes.noaa.gov/HURRLOOPS/huwvloop.html
"Example: the urban boundary layer. Cities exert their own influence on the boundary layer. The Earth-atmosphere interface in a city tends to be drier and rougher than areas of open land. In addition, the nature of man-made building materials means that they tend to respond rapidly to solar heating (G and c). Since the surface is dry, the latent heat flux into the air is small, so energy passes into the boundary layer in the form of sensible heat. This creates the `urban heat island' effect: the city tends to be warmer than the surrounding rural areas. Under low winds, a circulation similar to the sea breeze results, during the day, with cool air entering the city. This may cause pollution to converge on the city region. Under stronger winds, the high roughness length of the urban area causes relatively strong drag, leading to a deflection of the winds to the left (northern hemisphere). Generation of turbulence by the roughness tends to keep the boundary layer well-mixed, which means that a nocturnal inversion, with cold surface temperatures, is less likely to occur in an urban area."
If this is true, and the urban heat island could by the resulting turbulance in a city cause the boundary layer to be well mixed..doesn't that promote the capping effect that could restrict storms from building?
If I am crazy..let me know.
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I was afraid today the storms would be worse, now that the low's tail is drawing from the gulf.
Anyway, as you can see it shouldn't be so bad tomorrow.
What would cause that split? Heat island? If so..why?
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Once Melbourne was built up, as the seabreeze rolled by (ussually in the mid to late morning), it would have a gap over our developing heat island. I'm not sure but I think Lake Washington (just west of Melb), St Johns river & a lot of swamp to the west plays a roll ~ stong east wind hits extra heat (from the heat island), the clouds rise, then hits the cooler air like a wall perhaps. They do circle back around as they rise. To the south, the clouds curve S back to E, N & W again, just exploding many times before the whole line moved west. The N side of me would do the same thing but spin clockwise while building. We'd get warm wind, sometime blue sky right over head & maybe a little rain.
As the years went by new areas were built N of here, Suntree & Viera. Those areas stopped taking such a beating. Just north of there Cocoa, Rockledge & Titusville have been for a long time & had grown as well. The gap got wider as Mims, just north of Titusville & still rural, now takes a much larger brunt on a regular basis. To the south as Palm Bay has grown they are taking a little less beating (their not quite to the heat island standards of developement obtained here). The brunt has move to the next rural town south, Malabar.
On days that the clash happens with the west coast breeze & moves back this way, if we had no rain earlier, which many times now it the case, we get a beating many times since it's become so hot by late afternoon.
The hail is raging on though in mostly AL. Not 45 mins ago 4 1/4" hail in Marshall county AL.
Sure hope today is better than yesterday was as far as the sever thunderstorms, hail, and tornadoes go.
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