Robert Dewey
EF5
I'm still thinking there is a slight chance for a heavy snow event across portions of the Great Lakes tomorrow. Models are STILL showing QPF in excess of an inch, much of which falls in a 6-8 hour period of very intense omega. Since all of the models show the same thing, and the radar echoes and IR cloud tops are blossoming, I don't think models are doing all that bad in the QPF department.
Snow growth actually looks very good with the best omega and RH values centered at -22C... CSI and even CI is present (and quite strong) along the axis of the TROWAL, again - within the best omega, RH, and temp range.
The big question is precipitation type. I still don't think it's clear cut... The 7PM obs showed snow at Hillsdale, and mixed precipitation at Port Huron (maybe errors?) - and this is the WARMEST the profile will be for the next +36 hours. In fact, ACARS data for 00Z shows only a very slim warm layer across areas of south central MI (near Hillsdale). If the atmosphere can support snow within moderate precipitation rates, what will happen tomorrow during a period of very heavy precipitation rates? I would think dynamic cooling (NOT evaporational cooling) would allow for all snow. There is still a good 2.5 inches of snow on the ground here with 0.75 inches of water equivalent... That will be pretty hard to melt with temps remaining in the mid 30's (34F right now).
I really think this is a go big or go home event... If precipitation rates don't materialize - things will be rain. If heavy precipitation does occur, it would probably be in the form of snowfall. Just how much snow would depend on where the axis of heaviest QPF sets up, how much QPF, and whether or not dynamic cooling can overcome the SFC to 1KFT AGL warm layer.
Here are a few case studies in which dynamic cooling caught forecasters off guard:
http://www.crh.noaa.gov/lmk/soo/sclimo/evt...t_jan171994.php
http://www.srh.noaa.gov/topics/attach/html...ml/ssd98-10.htm
Snow growth actually looks very good with the best omega and RH values centered at -22C... CSI and even CI is present (and quite strong) along the axis of the TROWAL, again - within the best omega, RH, and temp range.
The big question is precipitation type. I still don't think it's clear cut... The 7PM obs showed snow at Hillsdale, and mixed precipitation at Port Huron (maybe errors?) - and this is the WARMEST the profile will be for the next +36 hours. In fact, ACARS data for 00Z shows only a very slim warm layer across areas of south central MI (near Hillsdale). If the atmosphere can support snow within moderate precipitation rates, what will happen tomorrow during a period of very heavy precipitation rates? I would think dynamic cooling (NOT evaporational cooling) would allow for all snow. There is still a good 2.5 inches of snow on the ground here with 0.75 inches of water equivalent... That will be pretty hard to melt with temps remaining in the mid 30's (34F right now).
I really think this is a go big or go home event... If precipitation rates don't materialize - things will be rain. If heavy precipitation does occur, it would probably be in the form of snowfall. Just how much snow would depend on where the axis of heaviest QPF sets up, how much QPF, and whether or not dynamic cooling can overcome the SFC to 1KFT AGL warm layer.
Here are a few case studies in which dynamic cooling caught forecasters off guard:
http://www.crh.noaa.gov/lmk/soo/sclimo/evt...t_jan171994.php
http://www.srh.noaa.gov/topics/attach/html...ml/ssd98-10.htm