Jon Miller
EF2
Can there be too much wind shear and , if so, what are the limits for tornadic storms ? Are there any good web sites that discuss wind shear and how it is deterrmined, etc?
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[Broken External Image]:http://www.crh.noaa.gov/techpapers/service/tsp-10/fig6.jpg
Figure 6. Scatter diagram showing combinations of CAPE in J/kg and 0-2 km AGL positive wind shear for 242 tornado cases during 1980-1990 (Johns et al. 1993). Figure reproduced from Johns and Doswell (1992).
Originally posted by Jeff Snyder
Amos,
I think we need to be careful about drawing conclusions relating tornado frequency to a combination of helicity and CAPE.
Originally posted by Amos Magliocco
I think the results suggest that a particular environment of CAPE and SRH supports more strong tornadoes than other sets of those particular values. Nothing more and nothing less. But it seems germane to the idea of too much shear.
Originally posted by Jeff Snyder+--><div class='quotetop'>QUOTE(Jeff Snyder)</div><!--QuoteBegin-Amos MaglioccoI think the results suggest that a particular environment of CAPE and SRH supports more strong tornadoes than other sets of those particular values. Nothing more and nothing less. But it seems germane to the idea of too much shear.
But does it? Saying so means that one can conclude that there's a better chance of a strong/violent tornado occuring with a 300 0-2km helicity and 3000 CAPE combination than with a 500 0-2km helicity and 5000 CAPE combination. [/b]
Originally posted by Gabe Garfield
In my observation, extreme instability with moderate shear is much better than the volatile extreme instability/extreme shear combo.
Gabe
Extreme CAPE and extreme instabilty just don't coexist very often - so if you have an example when it happened, I'd be interested in hearing about it (seriously).
You probably noticed the sounding at OAX still had a healthy cap of 50 J/Kg, and what we see is that storms were developing north of a boundary at the surface, where temps were only in the 70's, so convection was not occuring in the region with both large CAPE and large shear.
Originally posted by Glen Romine
Sounds like you are confusing environments favorable for discrete vs. linear convective modes, which is not the same as favorable environments for tornadoes.
Soundings are just too far apart, and launched too rarely to capture these rare meetings with any real frequency.
Can you give even one example?
THE AIR MASS IS EXTREMELY UNSTABLE AND THE DEEP LAYER SHEAR
IS FAVORABLE FOR TORNADIC SUPERCELLS.
Cap strength does not regulate storm mode in any formulation that I've ever seen. Sounds like you are confusing environments favorable for discrete vs. linear convective modes, which is not the same as favorable environments for tornadoes.
When forecasting a threat of tornadoes, the mode of convective initiation and the number and spacing of supercells that form are critical to the number of tornadoes expected. In the same mesoscale region, several supercells may develop in association with different forms of boundaries. These boundaries vary in detectability when using conventional data sources, and storms may form where there are no apparent boundaries. The initial storms in the 3 May 1999 outbreak evolved into tornadic supercells that each lasted several hours, with no early transition to a squall line or other convective mode. Storm spacing and motions were such that the supercells remained in an environment of favorable vertical shear and instability for several hours without numerous storm collisions, thus allowing the supercells to produce a large number of tornadoes.
The predominance of a supercell convective mode and lack of a squall line on 3 May 1999 may have been attributable to the lack of strong low-level convergence near the dryline(s). It is conceivable that the outbreak would not have materialized in such intense or prolific form had the convergence been stronger along a consolidated dryline, and had numerous storms formed simultaneously and merged into a larger-scale convective system in the weakly capped environment over northwestern Texas and western Oklahoma during the afternoon.
Originally posted by Jeff Snyder+--><div class='quotetop'>QUOTE(Jeff Snyder)</div>LOL I've got a good case for a combo of high low-level shear + strong instability...
[Broken External Image]:http://www.tornadocentral.com/now/July210z02MPXsounding.gif
0z July 21, 2002, MPX sounding... The tornado reports are empty because the cap held any deep moist convection at bay this day. I haven't seen too many soundings which show ~5800 J/kg MLCAPE (>6100 SBCAPE) and 262 m2/s2 0-1KM SRH (404 0-3km)... This may have been a good day to see this discussion at work considering that the deep layer shear (0-6km) was not terribly impressive at 40kts.
<!--QuoteBegin-Glen RomineSounds like you are confusing environments favorable for discrete vs. linear convective modes, which is not the same as favorable environments for tornadoes.
I know this comment was directed at Gabe's post, but I just had to interject here... I think there is a pretty strong relationship between storm mode and tornado occurrence, and I don't htink many here would argue that there isn't a relationship between the two. I think storm mode is incredibly important to tornado potential... Yes, environments that are most likely to directly affect tornadoes (mainly low-level shear) are not directly associated with storm mode (e.g. squall lines, supercells, etc) and vice versa. But I do think that the parent mesocyclone plays a very important role in the development of tornadoes given strong low-level shear. Again, I know you're probably saying that we can't really use 0-6km shear for tornado forecasting and 0-1km/0-3km helicity for supercell forecasting, but the 0-6km shear does play a role in storm rotation most likely, which in turn can aid in tornadogenesis if you take the theory of tilting and stretching of streamwise vorticity. This is neglecting the fact that updraft rotation in general can significantly enhance updraft 'strength'/velocity relative to a nonrotating updraft...[/b]
Originally posted by Mike Hollingshead
LOL, I can assure you that was not north of the boundary in cool air. Look closer at your sfc temps and where those storms are. Hell that one return is almost on O'Neill at 7pm and O'Neill is 91/63. That would be this storm maybe 1hr later north of Norfolk.
Originally posted by Jeff Snyder+--><div class='quotetop'>QUOTE(Jeff Snyder)</div>Thanks Jeff. I'll take a look at this later... you guys are overwhelming me a bit with all this at once.....LOL I've got a good case for a combo of high low-level shear + strong instability...
[/b]
<!--QuoteBegin-Jeff Snyder
I know this comment was directed at Gabe's post, but I just had to interject here... I think there is a pretty strong relationship between storm mode and tornado occurrence......
With stronger shear setups, storms tend to form convective lines and complexes rather than isolated cells. Most high shear/low instability tornado days feature fairly discrete storms (not always the case, but generally speaking). Storm mode is highly dependent on the orientation of the shear vector (relative to the pertinent storm initiating boundaries) and also on the cap strength.
Again - are talking about deep layer shear or low-level shear? If you have too strong of deep layer shear for the amount of buoyancy present - storms are simply ripped apart - so you have no storms at all. If the statement here is that you can have too strong of low-level shear, that doesn't hold either. Deep layer shear combined with the amount of buoyancy regulates the type storm that will occur. If you have extreme CAPE, you don't need the as much deep layer shear (example - Jarrell Tx. 27 May 1997 F5), likewise, with extreme low-level shear you can get strong tornadoes with surprisingly little buoyancy (example Van Wert Oh. 10 November 2002 F4). Go back and look at this case - there was LOTS of forcing. That is what is shown in the Johns and Doswell plot, and really nothing more than there is a very broad range of favorable combinations of low-level shear and buoyancy.I think that extreme shear is good only in cases where the overall forcing for convection is weak
In my observation, extreme instability with moderate shear is much better than the volatile extreme instability/extreme shear combo.
Originally posted by Gabe Garfield+--><div class='quotetop'>QUOTE(Gabe Garfield)</div>Are soundings necessary to determine instability/wind shear parameters? There are a number of other methods for determining these quantities (satellite, wind profilers, etc.).
[/b]
These are valuable tools for estimating the environment, but are no substitute for the real thing. Satellite soundings use model output for the first guess, use lot's of assumptions to come up with the profile, and have large error bars. While problems are being solved in this field quickly, they have a long way to go imo.
You could add hodograph curvature as being equally important. Large curvature favors one updraft over the other after the required split from tilting of environment horizontal vorticity, allowing for streamwise ingestion of the environment shear. If you have a straightline hodograph, then cell splitting is likely, and possibly deconstructive cell interaction and merging of cold pools that force more convective initiation and rapid transition to a squall line. The Edwards and Thompson paper you quoted notes the importance favorable shear and instability - and a weakly capped environment!!! So, a strong cap is not mentioned as a favorable characteristic of this case.Originally posted by Gabe Garfield+--><div class='quotetop'>QUOTE(Gabe Garfield)</div>I'm a modeler - so I'd love to say yes, but I can't.Does model initialization from 00z 24 May 2004 count? As I recall, CAPE was well over 4000 j/kg.
[/b]
<!--QuoteBegin-Gabe Garfield@
Cap strength does not regulate storm mode? Maybe not by itself, but a stronger cap means fewer storms and less storm mergers (e.g. change in storm mode).
<!--QuoteBegin-Gabe Garfield
As far as 0-6 km shear determining storm mode, I can think of at least one exception from '04. Large 0-6 km shear was present in C. OK on May 29th (C. OK was under the mid-level jet), yet the storm mode was high precipitation for a good part of its lifespan.
So, a strong cap is not mentioned as a favorable characteristic of this case.