Dr. Jeff Masters' WunderBlog

Grading NHC's Tropical Weather Outlook
Posted by: Dr. Jeff Masters, 4:33 PM GMT on June 06, 2007 +4
The National Hurricane Center's Tropical Weather Outlook (TWO) is a text-only product that rates the potential of disturbed areas of weather to turn into tropical depressions or tropical storms. The outlooks are issued four times daily, at 5am, 11am, 5pm, and 11pm EDT. I've found them to be an excellent guide to what to watch out for. But how accurate are these outlooks? To find out, Jamie Rhome and Dan Brown, who are two of the hurricane specialists that write the Tropical Weather Outlook, verified the accuracy of all the outlooks issued in 2005 and 2006. They used a three-tiered classification of threat based on the following language appearing in the TWO:

High: "A tropical depression could form tonight or the next day."

Medium: "Some slow development is possible."

Low: "Tropical storm formation is not expected."


These forecasts were then graded by looking at the "best track" database of Atlantic hurricanes and seeing if a tropical depression formed within 48 hours of each TWO issued. The results, shown below, reveal that for the Atlantic in the years 2005 and 2006:

-When the TWO said, "A tropical depression could form tonight of the next day," a depression formed within 48 hours 53% of the time.

-When the TWO said, "Some slow development is possible," a tropical depression formed within 48 hours about 20% of the time.

-When the TWO said, "Tropical storm formation is not expected," a tropical depression formed within 48 hours only 3% of the time.




Figure 1. Verification of the Atlantic and Eastern Pacific Tropical Weather Outlooks issued in 2005 and 2006. Image credit: Jamie Rhome and Dan Brown, National Hurricane Center.

Jeff Masters
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1851. seminolesfan 6:32 PM GMT on June 10, 2007    
Posted By: jphurricane2006 at 6:29 PM GMT on June 10, 2007.
lol seminolesfan

im not saying it wont develop, just needs some more deep convection

and in my opinion its much harder for a system to obtain and maintain structure and circulation then it does convection


but without convection there is nothing to maintain the low pressure center either, which was the cause for it's invest originally.

Gotta have the PB and the J to make a good sammich!!
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1853. seminolesfan 6:39 PM GMT on June 10, 2007    
I'm not arguing w/ ya there. A structured wave is waaaay sexier than an androgenous blob. My point is only that the structure cannot survive on its own accord. Without some energy that structure won't maintain itself indefinatly.
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1854. Chicklit 6:39 PM GMT on June 10, 2007    
What is different about this year, or this particular wave, that makes it perform in such an unusual manner? The wave before it looked almost as great coming off Africa, but it fizzled right away. Why didn't this one?

Brings to mind a discussion about the rainier-than-last-year season in Africa having an effect on the amount of African dust (a storm killer).
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1856. seminolesfan 6:41 PM GMT on June 10, 2007    
I think we're both looking at this the same way.

All I was saying is without convection the clock is ticking down faster than if there was some.
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1857. moonlightcowboy 6:41 PM GMT on June 10, 2007    
.
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1858. seminolesfan 6:44 PM GMT on June 10, 2007    
More chance of genesis well East of VA and Penn than for 93L...anyone else notice that. ROFL
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1859. hurricane23 6:46 PM GMT on June 10, 2007    
NHC 2:05PM Discussion on 93L....

A LARGE TROPICAL WAVE LOCATED S OF THE CAPE VERDE ISLANDS ALONG
23W/24W S OF 14N MOVING WEST NEAR 25 KT. A 1010 MB LOW IS
EMBEDDED ON THE WAVE AXIS NEAR 9N23.5W. UNFAVORABLE
UPPER-LEVEL WINDS...COOLER WATER TEMPERATURES...AFRICAN
DUST...AND A FAST MOVEMENT WILL HAMPER FURTHER DEVELOPMENT OVER
THE NEXT DAY OR TWO. DEEP CONVECTION ASSOCIATED WITH THIS
SYSTEM IS BASICALLY OVER TWO AREAS. SCATTERED MODERATE
CONVECTION IS FROM 10N-13N BETWEEN 25W-27W...AND FROM 5N-7N
BETWEEN 22W-26W.

NHC discussion on the scattered convection in the western caribbean.2:05pm also.

A TROPICAL WAVE IS IN THE WRN CARIBBEAN ALONG 80W S OF 16N
MOVING W NEAR 15 KT. ABUNDANT DEEP LAYER MOISTURE AND
CLOUDINESS OVER THE SW CARIBBEAN IS MAKING IT DIFFICULT TO
DEPICT LOW CLOUD MOTIONS IN THE AREA. THERE APPEARS TO BE SOME
CYCLONIC TURNING IN THE VICINITY BUT THIS MAY BE MORE ASSOCIATED
WITH THE NORMAL BACKGROUND FLOW AROUND COLOMBIA. SCATTERED
MODERATE TO STRONG CONVECTION IS NEAR JAMAICA FROM 16N-19N
BETWEEN 75W-78W. WIDELY SCATTERED MODERATE CONVECTION IS
FURTHER S FROM 12N-16N BETWEEN 76W-78W. SOME OF THIS CONVECTION
MAY BE MORE ASSOCIATED WITH DIFFLUENT FLOW ALOFT AHEAD OF THE
UPPER LOW OVER WRN CUBA.
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1860. moonlightcowboy 6:59 PM GMT on June 10, 2007    
Link

93L seems to be holding it together despite needing more convection, punching through some dust. If it stays weak, but together, won't it slide more west than north, making it more formidable?

...plus, look at all that mess coming "Out of Africa." Makes it looks like the Verdes will be shooting at us earlier and frequently!!!

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1861. Patrap 7:08 PM GMT on June 10, 2007    
GOES WV Loop of Tropical Basin
Link
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1862. Patrap 7:11 PM GMT on June 10, 2007    
Split-Window Meteosat-8 SAL


Link













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1864. stormpetrol 8:27 PM GMT on June 10, 2007    
Is there a low level spin more to the south and west of that blob of convection over and east Jamaica? I think I see one on vis sat imagery could be completely wrong though.
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1865. eye 8:32 PM GMT on June 10, 2007    
Bahurrican, show me which post i said anything like what you posted below. I have NEVER called anyone names like that....when someone mentions a eye forming in a wave, I joked...ok, pinhole...but never did i call anyone "stupid" in a thread....you need to correct your error.

Kyle & Eye: Just agree 2 disagree and leave it at that.

Eye - if u'd just leave off the personal comment at the end (e. g. "what are u, stupid?") what u have to say would be on target for the board.


As far as the tropics, does not appear Chantal will happen until early July at the earliest. We had the same thing happen last year with Africa this time, big huge waves that went "poof" and then when the CV season started, was just normal or below...

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1866. BahaHurican 8:36 PM GMT on June 10, 2007    
Here is a EUMETSAT Dust Image. The light and dark pink areas are dust. Dark red areas are high clouds (basically storm systems).

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1867. IKE 9:02 PM GMT on June 10, 2007    
eye said...

"As far as the tropics, does not appear Chantal will happen until early July at the earliest."........

How do you know that? That's a month away? What are you basing that on?
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1868. stormpetrol 9:08 PM GMT on June 10, 2007    
Despite the ULL to west of the convection around Jamaica and in the Southern Caribbean,I still think this area warrants monitoring, wouldn't surprise me at all if something more significant blossoms in a day or two.
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1870. WPBHurricane05 9:13 PM GMT on June 10, 2007    
Statement as of 5:30 PM EDT on June 10, 2007

For the North Atlantic...Caribbean Sea and the Gulf of Mexico...

Shower and thunderstorm activity has diminished in association with
a tropical wave located about 425 miles southwest of the Cape Verde
Islands.

Elsewhere...tropical cyclone formation is not expected during the
next 48 hours.

$$
Forecaster Blake
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1873. IKE 9:20 PM GMT on June 10, 2007    
That ULL appears to be moving west-southwest and should be out of the way within a day or 2.

Here's the unreliable 18Z NAM model run..has a 1000mb low in the NW Caribbean in 84 hours....

Link
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1877. BahaHurican 9:29 PM GMT on June 10, 2007    
On the dust around 93L, the full-disk imagery from which that dust photo is taken shows a dust storm over the Western Sahara (what did Dr. M call the area again?) which I am assuming will increase the amount of dust in the eastern ATL as the week progresses . . .
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1878. IKE 9:29 PM GMT on June 10, 2007    
Is The Weather Channel still discounting the SW Caribbean blob?

The shear outlook for the western Caribbean is favorable from tomorrow through Wednesday according to WU shear maps.
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1880. BahaHurican 9:36 PM GMT on June 10, 2007    
I think 93L is fascinating in its own right, simply by way of its appearance / structure and location at this time. It doesn't matter so much to me right now whether it has the chance to develop. I'm interested in what's happening with it RIGHT NOW . . . .

Think about Vince and Epsilon. Does the storm have to threaten land to be interesting?
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1882. KYhomeboy 9:48 PM GMT on June 10, 2007    
I agree. 93L is fascinating in its own right. I'm quite impressed that the wave signature is still so strong...even though deep convection is almost absent. If it can hold together for a day or too....conditions may become more favorable. Still...very interesting whether it's near land or not
1883. moonlightcowboy 9:51 PM GMT on June 10, 2007    
Excellent point, Baha. And, like the board has posted much today, there is landfall possibility, even if it's minute.

A few posts today maintain if the system stays weak, its chances to move more west are likely. A strengthening would lend to Coriolus curving her out out to sea. What will shear be like as the storm approaches 50w? SST appear to be warmer then and an environment for general strenthening as well.

At that point, wouldn't there be some landfall concerns? Just curious, Baha, what do you think?
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1885. Patrap 9:54 PM GMT on June 10, 2007    
Split-Window Meteosat-8 SAL
Link
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1886. HurricaneFCast 9:58 PM GMT on June 10, 2007    
moonlight- The Coriolis Effect has nothing to do with the direction in which storms move. It has everything to do with the way they rotate, and that's it. Coriolis is not anything that can "recurve a storm". It's simply the force that causes the counte-clockwise circulation in the Northern Hemisphere as well as the clockwise circulation in the Southern Hemisphere. I just do not want anyone to misunderstand the Coriolis Effect or Force as some people call it. This isn't a personal attack on you moonlight, so please don't take it that way...=)

In the case of direction of storms, however, the main culprit is the location of Low and High pressure systems as well as upper level winds.
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1887. kmanislander 10:11 PM GMT on June 10, 2007    
aroughleague

Pls resize your post. It is stretching the blog. 640 x 480 is a good size to use
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1888. BahaHurican 10:14 PM GMT on June 10, 2007    
aroughleague,

Can you reduce the size of your photo, please? Just add width and height specifications after the website address. For example

img src=http://oiswww.eumetsat.org/SDDI/html/images/out/SDDI-20070610-1900-RGB-09-DUST-04-1237.jpg height=500 width=500

inside the greater than / less than signs.

Thanks!
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1889. BahaHurican 10:18 PM GMT on June 10, 2007    
kman,

I would recommend a square resizing, since the orgininal photo looks like it was 1024x1024.

Did u get the BBQing done? (or was it a trip to the airport?)
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1890. kmanislander 10:19 PM GMT on June 10, 2007    
Baha

Patrap recommended I install Firefox because it automatically resizes outsize posts. My kids had it downloaded once but we took it off for some reason I cannot seem to remember now
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1891. IKE 10:20 PM GMT on June 10, 2007    
I'm using Mozilla Firefox...no problems on the size of aroughleague's picture. Ya'll must be on Internet Explorer.

Looking at the buoys in the western Caribbean...pressures are lower this afternoon then they were 24 hours ago and their around 29.80 to 29.85...and the water temps in the GOM have really gone up in the last week. Most buoys are reporting SST's in the mid 80's!
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1892. sporteguy03 10:21 PM GMT on June 10, 2007    
Actually convection might not matter right now for 93L but its structure to remain in tact, like the cake without the frosting, and besides the Navy is still watching it? That is why weather is fun and exciting because you never know and when you think you do you don't.
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1893. BahaHurican 10:21 PM GMT on June 10, 2007    
FCast,

Why did I think the Coriolus effect also had something to do with the overall flow of air along the equator? I am not saying it causes the curviture directly, but I'm thinking the upper air currents are somehow connected to this curling effect.

I need to go read some on this . . .
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1894. kmanislander 10:21 PM GMT on June 10, 2007    
Actually it was the airport. I have been back for a while but there hasn't been anything new to post on. I am still watching the area near 13N 77W as it has been attempting to refire with convection all day. The ULL has been keeping it in check but with that feature sliding off to the WSW the far S Caribbean may come under relatively low shear soon
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1895. Patrap 10:22 PM GMT on June 10, 2007    
reduce to 640 X 640 usually works well

Firefox2 download Link Now with spiffy new auto-spellchecker.
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1896. IKE 10:23 PM GMT on June 10, 2007    
Kman..it's suppose to be favorable in the western Caribbean Monday through Wednesday according to the WU shear maps.
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1897. kmanislander 10:23 PM GMT on June 10, 2007    
Ike,

I am on IE but as I said to Pat this morning there are many IE users on here and sizing is easy to do.
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1898. IKE 10:24 PM GMT on June 10, 2007    
I hear you.
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1899. Patrap 10:25 PM GMT on June 10, 2007    
Firefox needs to send me residuals..LOL
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1900. IKE 10:26 PM GMT on June 10, 2007    
LOL
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1901. kmanislander 10:27 PM GMT on June 10, 2007    
This is a close up of the area at those coordinates. It refuses to go away and this is where the "blob" over Jamaica today came from.
The ULL pulled the blob to the N and a new one looks to be trying to form here.
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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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