Iowa Flooding - Palo Iowa - The entire town of Palo Iowa was evacuated and was told to abandon due to flooding during the recent flooding of the the Cedar River and local water ways. During it's abandonment it was under military control. A week later the towns folk were allowed to re-enter their town to assess damage and begin clean-up. The town was devasted as you can see. Due to the fact the entire town was under water, their have been no coordinated efforts for donations, volunteer work, etc... plus, they've just been allowed back into their town and only during daytime hours. I'm sure they could use all the help they could get.
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This is Crown weather it shows all current and expected shear in the atlantic
GFS 850-200mb Shear Forecast
Shear can be expected to relax in the Eastern Atlantic with the development and expansion of a Sub Equatorial Ridge over the Cape Verde Islands and the weakening of the double barrel high pressure system in the South Hemisphere. Shear in the Caribbean should stay on the unfavorable side for the immediate future, according to the GFS forecast.
i think it's true that an existing strong storm can survive for a while in areas of low TCHP.
Wondering what in the world is going why the E-pac is now producing almost 3 TC'S well here is a small graphic showing what a favorable MJO can do as far as provide that extra spark meaning upward motion for tropical cyclone formation.As the favorable MJO moves into the GOM/Caribbean look for chances of development to go up in the first 2 weeks of july.
but...
I thought Strom died a couple years ago....
Flossie of last year rapidly intensified into a Category 4 in an area of low TCHP, so yes.
judging by the units, it almost seems that TCHP is measuring a flux, for lack of a better analogy, but without being time dependent.
so then how is TCHP measured? it should be related to the latent heat of vaporization of the water, right? i guess it all depends on which thermodynamic baseline value you choose for "0".
Using the 26 degree isotherm and the vertical depth of the isotherm the ocean waters.
We assume that vertical mixing is the only important effect on temperature during the passage of a tropical cyclone and ignore horizontal advection and surface heat exchange. Price (1981) demonstrates that surface temperature change is usually dominated by mixing, with cooling by surface fluxes a secondary factor. Under these conditions, the vertically integrated enthalpy remains constant:
- 0
|
| p Cp T dz
- -infinity
(sorry for the poor representation of calculus, but the figure wouldn't come out legible)
where Cl is the heat capacity of seawater, T is its temperature, and Ti is the initial temperature. In evaluating the integrals in (4), we approximate Cl and r as constants and, as illustrated in Fig. 1, we assume that the temperature lapse rate below the mixed layer is constant.
essentially, TCHP is the vertically integrated enthalpy of the water column based on some mixing and constant assumptions...
test
Indeed TerraNova, indeed! Did you also check it it's future porjected path bud?
So far the GFS has only completed it's run out to 168 hours, but it has it's Cape Verde system following the same general course as in previous model runs...along and around the southern edge of the high, which would fit the current steering pattern.
For days, it had the system. Yesterday, it dropped it completely (don't remember the exact run.) Today, it has it, barely as a closed low...
Here's the track to 180hrs:
The stronger that High is will also increase the wind shear as well....
The GFS shows a heavily sheared system moving north of Puerto Rico. Wind Shear is presumably why the GFS looses the system as it progresses further west.
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