Invest 95L,E of Bahamas,Comments,Sat Pics,Models Thread #1

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WindRunner
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#101 Postby WindRunner » Fri Jun 30, 2006 8:13 pm

HurricaneHunter914 wrote:http://cimss.ssec.wisc.edu/tropic/real-time/atlantic/winds/wg8sht.GIF

Shear should become favorable for development down the road.


I have been seeing shear maps used rather excessively this year, and people treating them like they were the bible of tropical cyclone development or something, and you have to remember that these maps can be inaccurate sometimes, by up to 20kts or so. These maps, whether computer or human generated, are subject to inaccuracies just like everything else in the weather world, and need to be taken into consideration with these thoughts in mind. From what I hear, a WV image is much more accurate when it comes to showing how badly a system is getting sheared. Of course this is somewhat more difficult to interpret, but it should lead to better conclusions as to the strength of the shear.
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#102 Postby cycloneye » Fri Jun 30, 2006 8:16 pm

wxman57,NRL adjusted the pressure upwards tonight to 1015 mbs from that 1009 mbs earlier this afternoon.And I agree with that upward pressure fix as pressures are high in that area as the Bahamas observations show.

http://www.nrlmry.navy.mil/tc_pages/tc_home.html

http://www.srh.noaa.gov/sju/caribm.html
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#103 Postby Noah » Fri Jun 30, 2006 8:30 pm

Is south west florida about to get pounded with rain again this weekend like what alberto did on june 12th??
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#104 Postby skysummit » Fri Jun 30, 2006 10:27 pm

I don't guess we'll get any 18z models?
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#105 Postby Noles2006 » Sat Jul 01, 2006 12:43 am

arcticfire wrote:Why does there always seem to be some war when it comes to chance to devlope , who says it will and who says it won't , anyone who says yes is an "alarmist" anyone who says no is "wishing it won't".

Pro mets have a job to do and people to answer to about what they say will and won't happen. They walk a very fine line and choose their words very carefully for that reason. I have yet to see any pro mets downplay any system that eventually went on to something. Yet here we are again and the pro mets seem to be on the defensive trying to prove they do their job.

What I do see is a lot of people who think anyone who thinks something might develop are evil and jump all over them. Just because the pro's do not think something will develop is no reason to bash anyone who gets excited about a blob or chats about thinking they see a circulation. If you don't think it's going anywhere fine , but stop calling people alarmists.

*hopes off his soap box*

It's the tropical season people , relax , watch and discuss thats what this forum is for. Stop taking sides like each invest is a battle.


Sorry, but what started this was someone calling out the Pro Mets because they felt the Professionals were downplaying every system that has come up lately.
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#106 Postby wxmann_91 » Sat Jul 01, 2006 12:58 am

HurricaneHunter914 wrote:http://cimss.ssec.wisc.edu/tropic/real-time/atlantic/winds/wg8sht.GIF

Shear should become favorable for development down the road.


1) I don't use those shear maps often; again, shear should be a vector, not scalar, quantity. And as WR stated, they aren't really accurate.

2) I don't see any favorable shear even from that shear map.
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#107 Postby WxGuy1 » Sat Jul 01, 2006 2:01 am

WindRunner wrote:
HurricaneHunter914 wrote:http://cimss.ssec.wisc.edu/tropic/real-time/atlantic/winds/wg8sht.GIF

Shear should become favorable for development down the road.


I have been seeing shear maps used rather excessively this year, and people treating them like they were the bible of tropical cyclone development or something, and you have to remember that these maps can be inaccurate sometimes, by up to 20kts or so. These maps, whether computer or human generated, are subject to inaccuracies just like everything else in the weather world, and need to be taken into consideration with these thoughts in mind. From what I hear, a WV image is much more accurate when it comes to showing how badly a system is getting sheared. Of course this is somewhat more difficult to interpret, but it should lead to better conclusions as to the strength of the shear.


More importantly, shear is not an advective property and is often NOT static! Just because a "system" is forecast to move into an area that has little shear NOW does not mean that shear will remain low in that area LATER. In addition, the magnitude of shear does not necessarily 'advect'. Shear is the difference (dir and magn) of flow between two levels. If flow at one level changes, so does the shear. Oftentimes, winds at both levels change, creating situations where shear can change rapidly. This also means that minor errors in wind speed and direction in model forecasts can create major errors in vertical wind shear forecasts. We all know about the dearth of observations (both surface and aloft) in the tropics, so that adds yet another complication / caveat.

Why not examine 500mb and 850mb model output to get an approximation of shear 24+ hrs in advance? Looking at this evening's GFS output, it looks like a 250mb cut-off low move slowly off the southeast US coast, resulting in 20-35kt westerly flow. Any storm that moves westward in this environment will face strong upper-level storm-relative flow, yielding stronger shear (storm-relative shear, since environmental shear is independent of system motion). The 0z NAM output is stronger with this cut-off upper-level low, indicating 40-75kt 250mb northwesterly flow east of Florida in a couple of days. Again, I can't imagine seeing a tropical depression or storm in such an environment. A slightly better bet for an environment favorable for convective organization may present itself if the 0z NAM has it's way in a few days in the Caribbean, south of a cut-off high progged to develop. FWIW, the GFS shows northwesterly upperlevel flow across much of the Caribbean in 48-72hrs, which just goes to show the variability of upper-level forecasts.

Re: the previous discussion about some folks not "wanting" development... Maybe there are some, but there are also some that always "want" development. The fact of the matter is that, as has been mentioned previously, only a fraction of INVESTs become tropical cyclones. Many pro mets value their FAR (False alarm ratio), which means that many don't want to forecast a cyclone when one doesn't develop. So, they call them as they see them. It seems that some folks don't like this -- they want us all to be like JB and always mention the "possibility" of development. Sure, he may call some storms well, but how many times does he mention development only to not see any development? I'm not slamming JB, but let's all remember that tropical cyclone forecasting is extremely difficult, particularly cyclone genesis.

How many INVESTs have we had this year? How many posts contain nothing but "Wow, I bet this one will be Beryl!"? I think it's good that Storm2k mods are trying to increase the signal-to-noise ratio, but it's never bad to post a reminder of the golden rule of maintaining high quality -- before you post, ask yourself if others will benefit from your post. If you think they will, then post away. If you think they won't, use the Private Message system. It's just now July 1st, and we've had how many threads about non-cyclones? There've been thousands of posts about convective areas that aren't even tropical depressions... I'm not saying we shouldn't discuss these, but it's tough (and time consuming) to weed through all the one-liner and emoticon-only posts to get to the substance.
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#108 Postby SouthFloridawx » Sat Jul 01, 2006 3:15 am

ATLANTIC OCEAN...
THE UPPER RIDGE THAT DOMINATES THE GULF EXTENDS ACROSS FLORIDA
INTO THE W ATLC W OF 77W. THE UPPER TROUGH OVER THE W ATLC
EXTENDS FROM 27N71W INTO THE CARIBBEAN ACROSS NEAR THE WINDWARD
PASSAGE. THE TROPICAL WAVE IS BENEATH THIS UPPER TROUGH. BROAD
UPPER HIGH IS OVER THE W TROPICAL ATLC CENTERED NEAR 11N50W
EXTENDING INTO THE E CARIBBEAN AND A RIDGE AXIS EXTENDING N INTO
THE W/CENTRAL ATLC FROM PUERTO RICO TO TO 30N65W THEN NE BEYOND
33N62W. DIFFLUENCE OVER THE NE CARIBBEAN IS GENERATING
SHOWERS/SCATTERED THUNDERSTORMS S OF 23N FROM 63W-72W. A LARGE
UPPER TROUGH COVERS THE N/CENTRAL ATLC N OF 30N FROM 32W-54W
INDUCING AN UPPER TROUGH EXTENDING FROM 28N38W TO A PAIR OF
SMALL MID/UPPER LOWS NEAR 25N43W AND 22N49W. AN UPPER RIDGE
EXTENDS OFF THE COAST OF AFRICA NEAR 12N16W EXTENDING W TO 14N27W
AND COVERS THE REMAINDER OF THE ATLC. AT THE SURFACE...A BROAD
RIDGE COVERS THE ATLC N OF 10N E OF 65W ANCHORED BY A 1030 MB
HIGH N OF THE REGION.

$$
WALLACE
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#109 Postby NONAME » Sat Jul 01, 2006 5:56 am

All the convection is gone from this system.
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#110 Postby Frank P » Sat Jul 01, 2006 6:25 am

WxGuy1 wrote:
WindRunner wrote:
HurricaneHunter914 wrote:http://cimss.ssec.wisc.edu/tropic/real-time/atlantic/winds/wg8sht.GIF

Shear should become favorable for development down the road.


I have been seeing shear maps used rather excessively this year, and people treating them like they were the bible of tropical cyclone development or something, and you have to remember that these maps can be inaccurate sometimes, by up to 20kts or so. These maps, whether computer or human generated, are subject to inaccuracies just like everything else in the weather world, and need to be taken into consideration with these thoughts in mind. From what I hear, a WV image is much more accurate when it comes to showing how badly a system is getting sheared. Of course this is somewhat more difficult to interpret, but it should lead to better conclusions as to the strength of the shear.


More importantly, shear is not an advective property and is often NOT static! Just because a "system" is forecast to move into an area that has little shear NOW does not mean that shear will remain low in that area LATER. In addition, the magnitude of shear does not necessarily 'advect'. Shear is the difference (dir and magn) of flow between two levels. If flow at one level changes, so does the shear. Oftentimes, winds at both levels change, creating situations where shear can change rapidly. This also means that minor errors in wind speed and direction in model forecasts can create major errors in vertical wind shear forecasts. We all know about the dearth of observations (both surface and aloft) in the tropics, so that adds yet another complication / caveat.

Why not examine 500mb and 850mb model output to get an approximation of shear 24+ hrs in advance? Looking at this evening's GFS output, it looks like a 250mb cut-off low move slowly off the southeast US coast, resulting in 20-35kt westerly flow. Any storm that moves westward in this environment will face strong upper-level storm-relative flow, yielding stronger shear (storm-relative shear, since environmental shear is independent of system motion). The 0z NAM output is stronger with this cut-off upper-level low, indicating 40-75kt 250mb northwesterly flow east of Florida in a couple of days. Again, I can't imagine seeing a tropical depression or storm in such an environment. A slightly better bet for an environment favorable for convective organization may present itself if the 0z NAM has it's way in a few days in the Caribbean, south of a cut-off high progged to develop. FWIW, the GFS shows northwesterly upperlevel flow across much of the Caribbean in 48-72hrs, which just goes to show the variability of upper-level forecasts.

Re: the previous discussion about some folks not "wanting" development... Maybe there are some, but there are also some that always "want" development. The fact of the matter is that, as has been mentioned previously, only a fraction of INVESTs become tropical cyclones. Many pro mets value their FAR (False alarm ratio), which means that many don't want to forecast a cyclone when one doesn't develop. So, they call them as they see them. It seems that some folks don't like this -- they want us all to be like JB and always mention the "possibility" of development. Sure, he may call some storms well, but how many times does he mention development only to not see any development? I'm not slamming JB, but let's all remember that tropical cyclone forecasting is extremely difficult, particularly cyclone genesis.

How many INVESTs have we had this year? How many posts contain nothing but "Wow, I bet this one will be Beryl!"? I think it's good that Storm2k mods are trying to increase the signal-to-noise ratio, but it's never bad to post a reminder of the golden rule of maintaining high quality -- before you post, ask yourself if others will benefit from your post. If you think they will, then post away. If you think they won't, use the Private Message system. It's just now July 1st, and we've had how many threads about non-cyclones? There've been thousands of posts about convective areas that aren't even tropical depressions... I'm not saying we shouldn't discuss these, but it's tough (and time consuming) to weed through all the one-liner and emoticon-only posts to get to the substance.


This was one of the best posts I've ever read on Storm2K.... thanks for the touch of sanity Wxguy1...
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#111 Postby cycloneye » Sat Jul 01, 2006 6:51 am

WxGuy1,excellent words in your post.As Frank P pointed out,also I say it's one of the best posts I haved read since storm2k was created in October,2002.
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#112 Postby storms NC » Sat Jul 01, 2006 7:26 am

NONAME wrote:All the convection is gone from this system.



With a system that has not development will lose thier convectionat night and will build back up in the day time. That is caused by the environment it is in. You will see this afternoon that it will have the convectionat back. Just wait for a few more week for the waters to be wamer then we may have something to talk about. But for now just a rain maker.
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#113 Postby CrazyC83 » Sat Jul 01, 2006 9:10 am

They've been quite liberal on declaring invests lately. This doesn't seem to have much potential at all.
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#114 Postby cycloneye » Sat Jul 01, 2006 10:10 am

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