Dr. Jeff Masters' WunderBlog

Midwest flood price tag $8 billion; Extreme Weather magazine review
Posted by: Dr. Jeff Masters, 4:54 PM GMT on June 27, 2008 +2
The American Farm Bureau, a lobbying group that represents American farmers, estimated yesterday that crop damage from the Midwest's Flood of 2008 has amounted to $7 billion. More than half of this total--$4 billion--was in Iowa. Other states taking a hit from excessive wetness and flooding were: Illinois, $1.3 billion; Missouri, $900 million; Indiana, $500 million; Nebraska $500 million; and an additional $1 billion in remaining wet states. When added to the at least $1 billion in property damage the floods wrought (including $762 million in Cedar Rapids, Iowa), the $8 billion price tag of the Midwest Flood of 2008 ranks as the second most expensive U.S. non-hurricane flooding disaster on record. America's worst flood, the Midwest Flood of 1993, caused $26.7 billion in damage (adjusted to 2007 dollars).

The damage will continue to rise in coming days, as major flooding continues along the Mississippi and Missouri Rivers. A levee broke along the Mississippi just north of St. Louis this morning, sending flood waters towards the small town of Winfield. Heavy rains in excess of five inches have hit much of northern Missouri this week (Figure 1), and NOAA's Hydrometeorological Prediction Center is forecasting a high probability of heavy rain in the region today through Saturday morning. The culprit is a slow-moving low pressure system over Minnesota, which will drag a cold front through Missouri tonight. An additional 2-4 inches of rain will fall in some areas along the front. The additional rain should keep the Mississippi and Missouri Rivers in Missouri above flood stage for an extra day or two. Currently, these rivers are expected to reach their highest crests sometime between Monday June 30 and Wednesday July 2. The forecast looks somewhat drier for the Midwest next week, thankfully. The jet stream has regularly been taking a major dip southward into the Central U.S. the past two months, putting the favored track for rainy low pressure systems over the Midwest. The jet often gets "stuck" in a high-amplitude trough-ridge pattern which causes drought in one part of the country (California in this case) and floods in another. This "stuckness" often lasts for 3 months. The current 2-week forecast from the GFS and ECMWF models predicts a continuation of the "stuck" jet stream pattern, but decreasing in amplitude and sliding more to the east. This should result in the favored storm track moving more towards the East Coast, relieving flooding in the Midwest.


Figure 1. Precipitation for the 7 days ending on Friday, June 27, at 8am EDT. Image credit:NOAA.

Review of the new magazine, Extreme Weather
A beautiful new weather magazine called Extreme Weather has hit the bookstores this month. Published by Astronomy magazine, the new magazine features some truly spectacular weather photos, including a 12-page "Weathergallery" with awesome shots of tornadoes, lightning, floods, supercells, hail, hurricane winds, and waterspouts. The first article of the magazine features the equally fantastic photos of storm chaser Warren Faidley, who also happens to be the best writer among professional storm chasers, in my opinion. Additional articles in Extreme Weather include a balanced and interesting look at the hurricanes/global warming connection, plus some quality articles on dust storms, super cell thunderstorms, lightning, and the Great Galveston Hurricane of 1900.

Extreme Weather is not yet a regular publication; the editors are gauging interest to see if they wish to make it so. I whole-heartedly encourage them to do so--this magazine rocks! You can order a copy at their website, it's $7.95.

Tropics
It's quiet in the tropical Atlantic. There are no threat areas to discuss, and none of the models are forecasting tropical storm formation in the next seven days.

Jeff Masters
500 Year Flood 2008 (UlaratheBard)
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.
500 Year Flood 2008
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Categories: Flood
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1451. all4hurricanes 9:48 PM GMT on June 29, 2008    
Link
This is Crown weather it shows all current and expected shear in the atlantic
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1452. FLWeatherFreak91 9:51 PM GMT on June 29, 2008    
Crown Wx = amazing site. PROPS to anyone involved with it :)
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1453. Drakoen 9:52 PM GMT on June 29, 2008    
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1454. TerraNova 9:52 PM GMT on June 29, 2008    
Question: How does the shear look over the next 7-10 days in the Atlantic? Will it support a storm? Also, can someone give me a link to modeled shear forecasts?

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.

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1455. hurricane23 9:55 PM GMT on June 29, 2008    
.
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1456. pearlandaggie 9:57 PM GMT on June 29, 2008    
looks like the EPac storms may have to contend with some shear...

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1458. mississippiwx23 10:00 PM GMT on June 29, 2008    
Thanks all. So it looks decent over near Africa...interesting. But it doesn't look so great if the system were to more west-northwest.
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1459. pearlandaggie 10:01 PM GMT on June 29, 2008    
hey StormW....is there any correlation between TCHP and maximum potential intensity of a storm? in other words, can a strong storm (>Cat3) form in an area of low TCHP?

i think it's true that an existing strong storm can survive for a while in areas of low TCHP.
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1461. hurricane23 10:02 PM GMT on June 29, 2008    
Afternoon!

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.

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1465. pearlandaggie 10:07 PM GMT on June 29, 2008    
doesn't it seem a little counterintuitive? i mean, if the amount of energy available for formation is low (i.e., shallow warm water, or cooler waters, etc.), it would seem that the situation would "cap" the maximum potential intensity of any storm that might form.
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1466. pearlandaggie 10:08 PM GMT on June 29, 2008    
look at this mess...looks like road rash!

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1467. presslord 10:10 PM GMT on June 29, 2008    
only the South Carolinians my get this...

but...

I thought Strom died a couple years ago....
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1468. KoritheMan 10:12 PM GMT on June 29, 2008    
in other words, can a strong storm (>Cat3) form in an area of low TCHP?

Flossie of last year rapidly intensified into a Category 4 in an area of low TCHP, so yes.
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1469. pearlandaggie 10:12 PM GMT on June 29, 2008    
1467. i get it! LOL...i would have made a joke like that a while back, but i figured it would fall flat!
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1471. pearlandaggie 10:14 PM GMT on June 29, 2008    
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".

judging by the units, it almost seems that TCHP is measuring a flux, for lack of a better analogy, but without being time dependent.
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1472. CybrTeddy 10:14 PM GMT on June 29, 2008    
So, 23 are you thinking that Bertha might form here in a few weeks?
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1473. Drakoen 10:18 PM GMT on June 29, 2008    
1471. pearlandaggie 10:14 PM GMT on June 29, 2008
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.
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1474. GeoffreyWPB 10:18 PM GMT on June 29, 2008    
Record high "low" temperature for West Palm this morning...80...ugggggg
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1475. presslord 10:20 PM GMT on June 29, 2008    
speaking of SC...rammb seems to think there's soem remote chance of something popping offshore...How Come? What's it thinking?
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1478. TerraNova 10:30 PM GMT on June 29, 2008    
The latest run of the GFS model develops the Cape Verde system (unlike the 12z model), and is generally less aggressive with it than in previous runs (00z/06z) until it clears -40W. The latest run still has the wave emerging on Tuesday.
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1480. pearlandaggie 10:33 PM GMT on June 29, 2008    
think i found it... from Emanuel et al, 2004:


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
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1482. TerraNova 10:34 PM GMT on June 29, 2008    
1479. JFV 5:32 PM EST on June 29, 2008
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.
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1484. Drakoen 10:38 PM GMT on June 29, 2008    
The latest GFS 18z run is closely in line with the ECMWF 12z run.
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1486. nash28 10:39 PM GMT on June 29, 2008    
Not really buying the GFS....

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...

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1487. nash28 10:41 PM GMT on June 29, 2008    
When we actually have a closed Low off the coast of Africa, then I'll start watching the models...
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1488. Drakoen 10:41 PM GMT on June 29, 2008    
It holds the closed low until the resolution goes out @192hrs.
Here's the track to 180hrs:
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1491. nash28 10:45 PM GMT on June 29, 2008    
The stronger that High is will also increase the wind shear as well....
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1495. pearlandaggie 10:47 PM GMT on June 29, 2008    
does a stronger A/B high also increase surface wind velocities? if so, then the evaporative cooling effect on the sea surface may also intensify, reducing total TCHP
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1501. TerraNova 10:53 PM GMT on June 29, 2008    
1491. nash28 5:45 PM EST on June 29, 2008
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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About JeffMasters
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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