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Severe parameters for 6/18/2014 - NYC


Mikehobbyst

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Looking at the ECMWF, GGEM, and GFS models and averaging everything out:

CAPE = 2500-3500 - scattered severe

LI = -6 and -8 - very unstable

Shear = 35-45 knot - favorable too

Temp 88

Dew point 75

Favorable jet region placement

925 temp 24 C

850 mb temp 17 C

700 mb temp 7-8 C - weak EML looks present.

300 mb winds 35-45 knts WNW flow (SVR derecho is a slight risk)

500 mb winds 35 knts - WNW flow with energy

EML= weak one present - may push this to strong SLGT risk SVR event

 

If we had better low and mid level lapse rates it could be a moderate risk type of day. One other thing of concern is cloud debris and any earlier convection.

 

Wednesday is looking most favorable for scattered severe, and isolated significant severe.

 

My guess on probabilities like SPC for 6/18:

 

Wind: 30 percent on the cusp to possible small hatched 45 percent area just west of NYC.

Hail: 15 percent

Tornado: 5 percent

 

This looks better than anything we had last year, and better than yesterday 6/13.

 

 

Thursday through Saturday look backdoorish again...

We may have our first significant 4-5 day east coast heat ridge from 6/22 to 6/27, with first 90 maybe likely.

 

Please comment...

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Upton not too gung-ho on a big severe threat 

 

 

 

EXPECT ANOTHER MCS TO POSSIBLY IMPACT THE AREA TUESDAY  
NIGHT...FOLLOWED BY A COLD FRONT PUSHING THROUGH LATE WEDNESDAY.  
HAVE SLIGHT CHANCE POPS TUESDAY NIGHT...THEN CHANCE POPS WEDNESDAY  
AS A RESULT. ANY THUNDERSTORMS AHEAD OF THE COLD FRONT ON  
WEDNESDAY COULD BE STRONG TO SEVERE WITH 1500-2500 J/KG OF  
CAPE...THE PASSING OF A 25-30 KT LOW LEVEL JET JUST TO THE  
S...20-30 KT OF 0-6 KM SHEAR AND 1000-1250 J/KG OF DOWNDRAFT CAPE.  
A LIMITING FACTOR THOUGH IS THE HIGH CAPE TO SHEAR RATIO YIELDS  
BULK RICHARDSON NUMBERS GENERALLY OF 80+ WHICH FAVORS ALMOST  
EXCLUSIVELY PULSE CONVECTION.

 

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Upton not too gung-ho on a big severe threat

They are probably right, how many advertised severe threats have we seen materialize from NJ/PA all the way into LI the past several severe seasons? Probably just end up being severe storms away from NYC with scattered showers/storms NYC-East. Thats my honest opinion....

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They are probably right, how many advertised severe threats have we seen materialize from NJ/PA all the way into LI the past several severe seasons? Probably just end up being severe storms away from NYC with scattered showers/storms NYC-East. Thats my honest opinion....

 

I may have heard you mention it once or twice

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I may have heard you mention it once or twice

:lol: people think im a debbie downer but this is just from experience. My location is literally a convective graveyard. Has its own local microclimate, the other day when that line of storms came through i got a three minute downpour with no lightning/ thunder

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:lol: people think im a debbie downer but this is just from experience. My location is literally a convective graveyard. Has its own local microclimate, the other day when that line of storms came through i got a three minute downpour with no lightning/ thunder

People are tired of hearing about it. It's the same thing every day.
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The CAPE looks to be the highest for the Southern Mid Atlantic. So any thunderstorms for the Tri State will be isolated/scattered, due to the lower instability for the area.

things can still change either way - good idea to keep an open mind 3 days out - once again wouldn't surprise me if there are flash flood watches and warnings along with severe T- Storm watches and warnings issued once again

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:lol: people think im a debbie downer but this is just from experience. My location is literally a convective graveyard. Has its own local microclimate, the other day when that line of storms came through i got a three minute downpour with no lightning/ thunder

It actually made it to Nassau County in pretty good shape. I wasn't home at the time but the storms were pretty intense from what I was told. I'm surprised it all made it beyond the seabreeze line.

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The best chance of strong or severe t-storms is where we see forcing, instability,etc come together. We also might have pocket of enhanced shear with the shortwave passing over the area Wed afternoon:

Shear6zGFS.png

500mb6zGFS.png

Currently SVR parameters look pretty good today for our area including LI. However still south of us from CNJ on south has the best chance for more organzied convection. Instability doesnt look an issue area wide at all but we'll also have to keep an eye on the mid-level lapse rates as well....

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Currently SVR parameters look pretty good today for our area including LI. However still south of us from CNJ on south has the best chance for more organzied convection. Instability doesnt look an issue area wide at all but we'll also have to keep an eye on the mid-level lapse rates as well....

 

We'll have to see where our triggering mechanisms wind up. There will be some cap in place that might limit areal coverage. The GFS at least, still has steep mid-level lapse rates. West winds should keep sea-breezes from pushing inland.The NAM and ECMWF also seem to be showing some better instability and shear parameters this morning. I'm optimistic. But there is still a few days for timing and parameters to change here.

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Per NWS discussion activity should make it into the region after dark. Biggest limiting factor looks to be waning instability. An embedded shortwave is forecasted to cross the region overnight and act as a triggering mechanism.

 

On Tuesday, despite increased instability the atmosphere is forecasted to be capped at the mid-levels. The cap then erodes late in the day as an MCS or convective feature crosses the region.

 

In my opinion Wednesday looks to be the best chance at severe with a potent shortwave crossing the region, ample instability and good lapse rates. Limiting factor would be timing which is still an unknown.

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Per NWS discussion activity should make it into the region after dark. Biggest limiting factor looks to be waning instability. An embedded shortwave is forecasted to cross the region overnight and act as a triggering mechanism.

 

On Tuesday, despite increased instability the atmosphere is forecasted to be capped at the mid-levels. The cap then erodes late in the day as an MCS or convective feature crosses the region.

 

In my opinion Wednesday looks to be the best chance at severe with a potent shortwave crossing the region, ample instability and good lapse rates. Limiting factor would be timing which is still an unknown.

to better explain that the biggest possible limiting  factor in the immediate metro late tonight is the marine layer with the onshore flow expected

 

Tomorrow should be a fun day for severe enthusiasts ...........

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Sudden slight risk upgrade for tonight. High winds main threat:

...LWR MI/GRT LKS TODAY INTO TNGT...

BAND OF SEASONABLY STRONG /40-50 KT/...LARGELY UNIDIRECTIONAL WSWLY

FLOW ON SRN FRINGE OF LK MI UPR IMPULSE WILL SWEEP E INTO THE LWR

GRT LKS/WRN NEW ENGLAND BY EARLY TNGT...ACCOMPANIED BY AN

APPRECIABLE INCREASE IN MOISTURE /PW 1.50-1.75 INCHES/. LOW-LVL

CONVERGENCE ACROSS REGION WILL REMAIN WEAK...DOMINATED BY LAKE

BREEZE BOUNDARIES IN UPSTATE NY/NW PA AND...POSSIBLY...BY CONVECTIVE

OUTFLOW IN LWR MI. COMBINATION OF MODERATE TO STRONG SFC HEATING

/ESPECIALLY IN NY/ WITH INCREASING MOISTURE SHOULD BOOST SBCAPE TO

BETWEEN 1500 AND 2500 J/KG. COUPLED WITH EXPECTED LOW TO

MID-TROPOSPHERIC WIND PROFILES...SETUP MAY PROVE FAVORABLE FOR

STORMS ORGANIZED INTO FAST-MOVING...FORWARD-PROPAGATING LINE

SEGMENTS WITH DMGG WIND. WHILE THE GREATEST SVR THREAT SHOULD EXIST

FROM SE LWR MI EWD THROUGH SW ON INTO NW PA AND UPSTATE NY THROUGH

THIS AFTN...A MORE LIMITED THREAT FOR SVR WEATHER MAY CONTINUE INTO

THIS EVE AS FAR E/SE AS NJ AND SRN NEW ENGLAND.

post-187-0-52352600-1403010713_thumb.gif

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Sudden slight risk upgrade for tonight. High winds main threat:...LWR MI/GRT LKS TODAY INTO TNGT...   BAND OF SEASONABLY STRONG /40-50 KT/...LARGELY UNIDIRECTIONAL WSWLY   FLOW ON SRN FRINGE OF LK MI UPR IMPULSE WILL SWEEP E INTO THE LWR   GRT LKS/WRN NEW ENGLAND BY EARLY TNGT...ACCOMPANIED BY AN   APPRECIABLE INCREASE IN MOISTURE /PW 1.50-1.75 INCHES/. LOW-LVL   CONVERGENCE ACROSS REGION WILL REMAIN WEAK...DOMINATED BY LAKE   BREEZE BOUNDARIES IN UPSTATE NY/NW PA AND...POSSIBLY...BY CONVECTIVE   OUTFLOW IN LWR MI. COMBINATION OF MODERATE TO STRONG SFC HEATING   /ESPECIALLY IN NY/ WITH INCREASING MOISTURE SHOULD BOOST SBCAPE TO   BETWEEN 1500 AND 2500 J/KG. COUPLED WITH EXPECTED LOW TO   MID-TROPOSPHERIC WIND PROFILES...SETUP MAY PROVE FAVORABLE FOR   STORMS ORGANIZED INTO FAST-MOVING...FORWARD-PROPAGATING LINE   SEGMENTS WITH DMGG WIND. WHILE THE GREATEST SVR THREAT SHOULD EXIST   FROM SE LWR MI EWD THROUGH SW ON INTO NW PA AND UPSTATE NY THROUGH   THIS AFTN...A MORE LIMITED THREAT FOR SVR WEATHER MAY CONTINUE INTO   THIS EVE AS FAR E/SE AS NJ AND SRN NEW ENGLAND.

Lets go!

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look at this map of the entire event and tell me if that is a true northwest to southeast movement from beginning to end - next tell me the main directional movement from beginning to end using the curved lines

 

http://www.spc.noaa.gov/misc/AbtDerechos/casepages/sep71998page.htm

Its one event, which was a derecho. I think he was talking about general MCS' which usually tend to move from the NW and dive ESE

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look at this map of the entire event and tell me if that is a true northwest to southeast movement from beginning to end - next tell me the main directional movement from beginning to end

 

http://www.spc.noaa.gov/misc/AbtDerechos/casepages/sep71998page.htm

Since when is one event a proper example for all?

 

Look back to the 2012 mid-atlantic derecheo, clearly NW to SE?

 

12jun29_rpts_svrplot.png

 

120629_rpts.gif.png

 

It's a known fact that stronger convection turns right.

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From http://link.springer.com/article/10.1007%2FBF01592957

 

Abstract

Migration velocities of convective storms are summarized for six situations, with different environmental wind fields. Small-and medium-sized storms generally moved to left of the direction of, and at speeds somewhat less than, the vector mean wind in the troposphere. Large-diameter (ca. 20–30 km) storms generally deviated to the right, in proportion to their sizes and to the veering of wind with height. This behavior, and the tendency for large storms to move appreciably slower than the mean wind, are even more pronounced when giant clusters of thunderstorms are considered. An example is analyzed in which a multicellular storm, 80 km wide, moved 55° to right of the mean wind and with half its speed. This behavior results from a characteristic pattern of propagation, in which new cells tend to form on the general upwind side of the cluster, with the larger and more intense cells developing on its right flank. The individual cells move through the cluster, dissipating on approach to its advancing and left flanks. Preferential formation of cells toward the rear side of the cluster is shown to be compatible with the probable origin and trajectories (relative to the moving storm) of air ascending from the lower part of the subcloud layer. The sometimes-observed rapid movement of large multicellular storms to left of the mean wind is partly accounted for by an opposite (left forward flank) pattern of propagation.

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