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JP 2 8 SPATIAL DISTRIBUTION of TROPICAL CYCLONE  Form

JP 2 8 SPATIAL DISTRIBUTION of TROPICAL CYCLONE Form

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5. Similarly the Upstate regions near Greenville-Spartanburg averaged only 0. 33 inches and 2. 18 inches of rain fell in the GSP and CAE regions respectively Figures 4 and 5. In the Greenville-Spartanburg region the forecast skill for Frances was excellent for the HAS forecasters at the SERFC but fell behind the which indicated regional errors of 0. JP 2. 8 SPATIAL DISTRIBUTION OF TROPICAL CYCLONE INDUCED PRECIPITATION AND OPERATIONAL APPLICATIONS IN SOUTH CAROLINA R. Jason Caldwell Hope P. In...
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So what we're going to talk about now is the formation of tropical storms we know that tropical storms bring heat moisture, and they also spin so what we have here is we need to heat, so it's got to be temperature needs to be above 27 degrees Celsius we need moisture therefore they have to occur over an ocean where we've got lots of moisture and that ocean needs to have warmth up to about 60 meters in depth, and we also need the spin, so we're talking between 5 degrees north of the equator and 30 degrees north or south of the equator and that will allow the storm to spin so around about here we would get tropical storms forming we're over an ocean it's nice and warm as it's between the tropics, and it's far enough north to be able to spin, so we have here an area of low pressure because the air above the ocean just here is nice and warm it's being warmed by the nice warm deep sea and as that air warms it starts to rise, and it rises rapidly and that creates an area of low pressure at t

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