Quote:
Originally Posted by srfoskey
What are periodic impulses?
They seem to aid in higher than normal precipitation chances, but that's about all I can gather.
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Quote:
COOLER AIR ALOFT AND PERIODIC IMPULSES WILL ALSO AID IN HIGHER THAN NORMAL PRECIP CHANCES.
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From that sentence... Cooler air aloft helps increase instability with a warmer surface.
Impulse in physics, refers to a sudden surge of current. In this case they are referring to the upward motion otherwise known as lift. Lift happens with instability. So with the cooler air aloft and an unstable atmosphere, there will be periodic times when there is that extra upward motion (lift) to create heavier precip.
VERY hard to determine exactly where! That's why some spots will get more precip than thought or forecasted. Some Hi-Res short range models can help depict this by looking at certain parameters like the 700 vort. This is used during snowstorms as well to see where the heaviest snow will fall. But with sudden changes even "during" a storm, you have to stay on top of this parameter to see if the chances or intensity changes and even still, it might not happen as the model is depicting
This was from yesterday morning from NWS Boston. Got my eyebrow raised a couple times.
THETA-E?
ENHANCED ASCENT PER DIFFERENTIAL VORTICITY ADVECTION? (extra lift?)
FOCUS UPON THE MID-ATLANTIC LOW AND PROXIMITY TO S NEW ENGLAND...AS
TO WHETHER IT WILL MAKE AN IMPACT. WHEN WE CONSIDER A MID-LEVEL OPEN-
WAVE TROUGH AND ACCOMPANYING ENERGY YIELDING FALLING HEIGHTS ACROSS
THE REGION WOULD EXPECT THE MID-ATLANTIC LOW AND FRONTAL BOUNDARY TO
LIFT BACK N ALONG WITH HIGHER VALUES OF THETA-E. WITH N/NE QUADRANT
H8-6 FRONTOGENESIS BENEATH DECENT UPPER-LEVEL VENTING AND SOME LEVEL
OF ENHANCED ASCENT PER DIFFERENTIAL VORTICITY ADVECTION WOULD EXPECT
SOME OUTCOME ACROSS OUR AREA. SHOULD THE STRONGER N-IMPULSE THROUGH
THE BROADER CYCLONIC FLOW AND PARENT SURFACE COLD FRONT PUSH INTO S
NEW ENGLAND SOONER THERE COULD BE A GREATER MAGNITUDE OF DEFORMATION
ACROSS THE INTERIOR. WITH 23.0Z GUIDANCE THERE IS TOO MUCH VARIANCE
TO MAKE A DETERMINATION ON THE EXACT TIMING OF THE COLD FRONT. THIS
IS ALSO EVIDENT WITHIN TELECONNECTIONS. WHILE LESS-AMPLIFIED AS THE
PREVIOUS FORECASTER NOTED...THE GFS AND ECMWF HAVE BEEN IN SOME
INSTANCES OUT OF PHASE. AS A RESULT THERE IS LOW CONFIDENCE WITH
RESPECT TO THE MID-TO LATE-WEEK FORECAST.