BUT RIGHT ABOUT HERE WE HAVE TO CONSIDER AN UNIQUE AND LIKELY OVERLOOKED FACTOR TO THIS SYSTEM.
LET'S CONSIDER THE LOW FROM THE NORTH 1ST. IT'S CYCLONIC FLOW, AS IT MIGRATES SE-WARDS, COMING IN FROM THE WEST, WILL CONTINUOUSLY BRING A SE OR SOUTHERN FETCH OF AIR/WIND AHEAD OF IT. WHICH MEANS, FOR A PROLONGED TIME, EARLY IN THIS SEQUENCE AND BEFORE THE COASTAL MERG., THIS WILL BRING A LONGER PERIOD OF WARMER AIR INTO SOUTHERN NEW ENGLAND/NYC ETC.
SO CONSIDERING THIS, THAT WOULD MEAN A SE STEADY WIND IN SOUTHERN HUDSON VALLEY, NYC, LI, CT, MASS, RI ETC. ALSO WOULD CERTAINLY PROLONG RAIN IN THE LOWEST ELEVATION TOPOGRAPHY OF THE SOUTHERN NEW ENGLAND REGION TOO (CONSIDERING THE HUDSON VALLEY IN EASTERN NY TOO). ON THE FLIP SIDE THOUGH, THERE'S PLENTY OF TYPICALLY COLD AIR AROUND, WITHOUT ALSO ADDING THE SOUTHERN CANADIAN COLD LOW'S REINFORCEMENT OF COLDER AIR TO THE REGION. THIS KINDA TRANSLATES INTO MORE AGREEMENT THAT HIGHER ELEVATIONS ARE GOING TO GET A CHANCE TO REALLY MAINTAIN COLDER AIR TEMPS LONGER, IF NOT ALTOGETHER. BUT THE KEY POINT HERE AGAIN, WE HAVE TO CONSIDER JUST HOW THE LAKES CLIPPER NUDGES THE ADVECTION PROCESS, AND TO WHAT EXTENT? TYPICALLY IT GENERALLY BRINGS SOUTHERN CT AIR INTO ALBANY, AND ENHANCED VIA THE HV WHICH IS DAMN-NEARLY SEA LEVEL WITH IT'S RIVER TIDES.
BUT THE FASTER THAT LOW GETS TO REDEVELOP,
OR EVEN BEGIN TO, OFF THE COAST,
THE FASTER THE TEMPS DROP AROUND THE SYSTEM TO MAKE IT'S NOR'EASTER MUCH MORE LIKELY!
NOW WE BEGIN TO CONCLUDE WE WILL LIKELY HAVE A RAIN AND MIX EVENT IN THE LOWEST ELEVATIONS, AND SOME PRETTY SERIOUS SNOW IN THE MTNS....AND, THE 2ND 1/2 OF THE EVENT WILL ALSO LIKELY BE ALL SNOW! HERE IS WHERE WE MAY ALSO BEGIN TO CONSIDER
'FEET OF SNOW'
POSSIBLE. AND THEN CONSIDER THE LOW TRACKING LIKE A BEMBLEBEE HITTING FLOWERS, WALLOWING ALONG, INSTEAD OF JUST BEE-LINING IT OUTTA HERE. WILL IT STAY CLOSE ENOUGH TO OUR CONTINENT TO CONTINUE SNOWING INLAND? JUST HOW FAR? AND 100 MORE QUESTIONS TOO. BUT.... LET'S TAKE A LOOK AT IT NEXT....
THE FOLLOWING IMAGE SHOWS THE LIKELY MATURED NOR'EASTER NOW. BUT WE NEED TO CONSIDER THE EVOLUTION OF A 'NOR-LUND TROUGHING' TO CONCENTRATE ON JUST WHO GETS THE INTENSE BOUNDARIES THAT SETUP, ASSOCIATED WITH INTENSE OR STRENGTHENING NORTHEAST WINTER SYSTEMS. THEY BASICALLY OUTLINE THE CONCENTRATED POST-OCCLUSION AREA OF THE SEQUENCE. THESE AREAS CONCENTRATE BANDS OF SNOW INTO VERY HEAVY TOTALS.