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Feb 11-12 "Potential"


phlwx

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Ralph

Not sure if it's excitement but it certainly could be a big problem. Briefly heavy snow high winds and falling temps with the road temps having been above freezing may very well equal quite the mess if someone gets the potential 1 to 2 inches of snow in a short time this evening.

Paul

I've never seen so much excitement over .01-.1 snow before in this forum.

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Ralph

Not sure if it's excitement but it certainly could be a big problem. Briefly heavy snow high winds and falling temps with the road temps having been above freezing may very well equal quite the mess if someone gets the potential 1 to 2 inches of snow in a short time this evening.

Paul

Paul,

I agree with you, but there is definitely a whim of excitement in the air in the thread. People are going to be caught somewhat off-guard, though the local news has been on top of this, so maybe not-so-much. Closing in on 2" here fwiw....

Steve

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Yeah, that was an impressive band that set up (February 3, 2009). Just for kicks, I went back to look up the post mortem I issued on this event the very next day. For those interested in reviewing it, here it is.

.POST MORTEM /FOCUSED HEAVY SNOW TUESDAY NIGHT/...

WELL, QUITE THE MESOSCALE EVENT UNFOLDED LAST NIGHT ACROSS THE LOWER

DELAWARE VALLEY. WHILE THE COASTAL STORM WAS WELL NORTHEAST OF OUR

AREA, A WELL DEFINED MID LEVEL SHORT WAVE SCOOTED ACROSS OUR AREA

WITH THE MAIN FOCUS ACROSS THE PHILADELPHIA METROPOLITAN AREA. THE

COMPUTER MODELS WERE INDICATING THAT A BANDED FEATURE WOULD

DEVELOP, HOWEVER THESE MESOSCALE FEATURES ARE TOUGH FOR THE MODELS

TO RESOLVE BECAUSE THEY ARE ON THE SMALLER SCALE AND DEPEND ON

CERTAIN VARIABLES COMING TOGETHER AT THE RIGHT TIME. HOWEVER,

THERE WERE SIGNALS THAT THIS COULD OCCUR BUT THE LOCATION WAS UP

IN THE AIR. IT TURNS OUT THAT THE FORECAST LOCATION WAS TOO FAR

NORTH WITH THE 12Z MODEL RUNS ON TUESDAY, BUT THE 18Z AND 00Z

MODELS BEGAN TO GET A BETTER HANDLE ON THE ORIENTATION AND

LOCATION OF THE INTENSE BANDED FEATURE. SO, WHAT CAUSED THIS?

THIS IS WHAT IS KNOWN AS A NORLUN INSTABILITY TROUGH. THERE WAS AN

INVERTED TROUGH AT THE SURFACE /VIA SURFACE OBSERVATIONS/ BENEATH

MIDLEVEL POSITIVE VORTICITY ADVECTION. THERE WAS A NARROW RIBBON OF

FRONTOGENETIC FORCING IN THE 925 MB TO 850 MB LAYER AND THERE WAS

INSTABILITY ALOFT. THE MAIN LIFT BECAME ORIENTATED NORTHWEST TO

SOUTHEAST ALONG AN INSTABILITY GRADIENT AS CONVERGENCE BECAME

MAXIMIZED ALONG THE TROUGH, WHICH LOOKED TO BE PLACED AT THE LEADING

EDGE OF THE POSITIVE VORTICITY ADVECTION. DOPPLER RADAR IMAGERY

SHOWED THAT THE SNOW SHIELD CONSOLIDATED INTO A MORE FOCUSED BAND

THROUGH THE EVENING AS MESOSCALE PROCESSES GOT UNDERWAY. A REVIEW OF

MODEL DATA VIA BUFKIT, INDICATED THE SNOW GROWTH REGION LOWERED

SUBSTANTIALLY IN THE EVENING WHICH LINED UP WITH HIGHER RELATIVE

HUMIDITY VALUES. BASED ON THE POSITION OF THE FRONTOGENESIS, IT

APPEARS THE LIFT WAS MAXIMIZED WITHIN A MUCH IMPROVED SNOW GROWTH

REGION, ALLOWING FOR EFFICIENT ICE CRYSTAL PRODUCTION. GIVEN THE

INSTABILITY THAT WAS IN PLACE, SNOWFALL RATES REACHED ABOUT 2

INCHES PER HOUR WITHIN THE HEART OF THE BAND AS THERE WAS A

CONVECTIVE CONTRIBUTION. THIS INTENSE SNOWFALL RATE WAS REPORTED

AT THE PHILADELPHIA INTERNATIONAL AIRPORT FOR A TIME. AS THE

ATMOSPHERE COOLED, THE SNOW TO LIQUID RATIO INCREASED AND PROBABLY

MAXED OUT TO ABOUT 20:1. AN INTERESTING OBSERVATION THAT WAS REPORTED

AT THE AIRPORT WAS THAT THE VISIBILITY DROPPED TO NEAR ZERO DURING

THE HEIGHT OF THE EVENT WITH A RUNWAY VISUAL RANGE AS LOW AS 600

FEET. NEEDLESS TO SAY, THESE TYPES OF EVENTS ARE DIFFICULT TO

FORECAST WITH A GOOD AMOUNT OF LEAD TIME. WHEN THEY DO OCCUR,

THERE IS A SIGNIFICANT IMPACT BUT IN A RELATIVE NARROW AREA, AS

THE SNOWFALL RATES ARE LOCALLY INTENSE. THE SETUP THAT OCCURRED

TUESDAY NIGHT DOES NOT HAPPEN OFTEN, BUT WHEN THEY DO, AREAS

UNDERNEATH THE BANDED FEATURE CERTAINLY GET A DUMPING OF SNOW.

AS A SIDE NOTE, THE LAST TIME PHILADELPHIA PICKED UP 8 INCHES OR

MORE OF SNOW DURING AN EVENT WAS FEBRUARY 11-12, 2006 WHEN 12.0

INCHES OCCURRED.

Never forget this event....my gf (now wife) and I had just moved locations within Woodbury after my first couple winters down here were rather meh. As we were moving in she commented that our 6 block move would put us in a more favorable position for snow so I could stop my whining. I laughed bitterly at the time and then rather happily 72 hours later as we jackpotted. As amazing as it was to have all those ingredients come together it was more amazing that they stayed focused over about 4-5 towns here in Gloucester county for so long.

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Give the Euro credit on this one (although it had in about 4 different states in 8 runs), taking the leap it will happen, never wavered.

Unfortuately I sense several mutli-vehicular accidents later today.

Thats a pretty strong statement...do you feel that strongly about the current NAM depiction or just overall concern of the flash freeze potential?

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Yeah, that was an impressive band that set up (February 3, 2009). Just for kicks, I went back to look up the post mortem I issued on this event the very next day. For those interested in reviewing it, here it is.

.POST MORTEM /FOCUSED HEAVY SNOW TUESDAY NIGHT/...

WELL, QUITE THE MESOSCALE EVENT UNFOLDED LAST NIGHT ACROSS THE LOWER

DELAWARE VALLEY. WHILE THE COASTAL STORM WAS WELL NORTHEAST OF OUR

AREA, A WELL DEFINED MID LEVEL SHORT WAVE SCOOTED ACROSS OUR AREA

WITH THE MAIN FOCUS ACROSS THE PHILADELPHIA METROPOLITAN AREA. THE

COMPUTER MODELS WERE INDICATING THAT A BANDED FEATURE WOULD

DEVELOP, HOWEVER THESE MESOSCALE FEATURES ARE TOUGH FOR THE MODELS

TO RESOLVE BECAUSE THEY ARE ON THE SMALLER SCALE AND DEPEND ON

CERTAIN VARIABLES COMING TOGETHER AT THE RIGHT TIME. HOWEVER,

THERE WERE SIGNALS THAT THIS COULD OCCUR BUT THE LOCATION WAS UP

IN THE AIR. IT TURNS OUT THAT THE FORECAST LOCATION WAS TOO FAR

NORTH WITH THE 12Z MODEL RUNS ON TUESDAY, BUT THE 18Z AND 00Z

MODELS BEGAN TO GET A BETTER HANDLE ON THE ORIENTATION AND

LOCATION OF THE INTENSE BANDED FEATURE. SO, WHAT CAUSED THIS?

THIS IS WHAT IS KNOWN AS A NORLUN INSTABILITY TROUGH. THERE WAS AN

INVERTED TROUGH AT THE SURFACE /VIA SURFACE OBSERVATIONS/ BENEATH

MIDLEVEL POSITIVE VORTICITY ADVECTION. THERE WAS A NARROW RIBBON OF

FRONTOGENETIC FORCING IN THE 925 MB TO 850 MB LAYER AND THERE WAS

INSTABILITY ALOFT. THE MAIN LIFT BECAME ORIENTATED NORTHWEST TO

SOUTHEAST ALONG AN INSTABILITY GRADIENT AS CONVERGENCE BECAME

MAXIMIZED ALONG THE TROUGH, WHICH LOOKED TO BE PLACED AT THE LEADING

EDGE OF THE POSITIVE VORTICITY ADVECTION. DOPPLER RADAR IMAGERY

SHOWED THAT THE SNOW SHIELD CONSOLIDATED INTO A MORE FOCUSED BAND

THROUGH THE EVENING AS MESOSCALE PROCESSES GOT UNDERWAY. A REVIEW OF

MODEL DATA VIA BUFKIT, INDICATED THE SNOW GROWTH REGION LOWERED

SUBSTANTIALLY IN THE EVENING WHICH LINED UP WITH HIGHER RELATIVE

HUMIDITY VALUES. BASED ON THE POSITION OF THE FRONTOGENESIS, IT

APPEARS THE LIFT WAS MAXIMIZED WITHIN A MUCH IMPROVED SNOW GROWTH

REGION, ALLOWING FOR EFFICIENT ICE CRYSTAL PRODUCTION. GIVEN THE

INSTABILITY THAT WAS IN PLACE, SNOWFALL RATES REACHED ABOUT 2

INCHES PER HOUR WITHIN THE HEART OF THE BAND AS THERE WAS A

CONVECTIVE CONTRIBUTION. THIS INTENSE SNOWFALL RATE WAS REPORTED

AT THE PHILADELPHIA INTERNATIONAL AIRPORT FOR A TIME. AS THE

ATMOSPHERE COOLED, THE SNOW TO LIQUID RATIO INCREASED AND PROBABLY

MAXED OUT TO ABOUT 20:1. AN INTERESTING OBSERVATION THAT WAS REPORTED

AT THE AIRPORT WAS THAT THE VISIBILITY DROPPED TO NEAR ZERO DURING

THE HEIGHT OF THE EVENT WITH A RUNWAY VISUAL RANGE AS LOW AS 600

FEET. NEEDLESS TO SAY, THESE TYPES OF EVENTS ARE DIFFICULT TO

FORECAST WITH A GOOD AMOUNT OF LEAD TIME. WHEN THEY DO OCCUR,

THERE IS A SIGNIFICANT IMPACT BUT IN A RELATIVE NARROW AREA, AS

THE SNOWFALL RATES ARE LOCALLY INTENSE. THE SETUP THAT OCCURRED

TUESDAY NIGHT DOES NOT HAPPEN OFTEN, BUT WHEN THEY DO, AREAS

UNDERNEATH THE BANDED FEATURE CERTAINLY GET A DUMPING OF SNOW.

AS A SIDE NOTE, THE LAST TIME PHILADELPHIA PICKED UP 8 INCHES OR

MORE OF SNOW DURING AN EVENT WAS FEBRUARY 11-12, 2006 WHEN 12.0

INCHES OCCURRED.

Thanks for this, very educational. Any thoughts on what to look for mid-afternoon on where this is setting up, if at all?

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Thats a pretty strong statement...do you feel that strongly about the current NAM depiction or just overall concern of the flash freeze potential?

Since this has convective elements, the geographic extent of the jackpot area is going to be too large, which plays into the "surprise" element too. Going from nothing to poor visibility and potentially snow covered roads plus those dropping below freezing temperatures.

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