Roy Niemann
I guess with the snow cover (.1 inch) it’s keeping the temerature to 23 degrees.
Jan 1996 we received over 35 inches of snow during a 3 day snowstorm. .It shut ev erytthing down for about a week.
Keep on posting Henry. You’ve been consistent aand that makes me trust your forecasts.
Henry as you said there may be “thumps” as JB called them. Here in Indiana PAA we are getting one right now. Up to 0.5 inches already
What is JB’s full name?
Joe Bastardi
Thank you!!! Much appreciated
Interesting. KDKA here in Pittsburgh is 90 degrees out of phase with your forecast for the winter. Monthly average temps about 1-1.5 degrees abovee normal. Snow totals 24 inches where the average is 40 innches for the entire winter. We shall see. Henry, I think you got it right.
It’s interesting, back in Philly aaround the 15th to the 30th of october we’d get a strong cold front with heavy rains signaling the start of real fall temperatures. I guess we can say this cold front is signaling the change over as you’ve been predicting Henry.
I see we’ve got some lightning to go with this cold front here in western pa. Signaling the cold air is finally avectcing?
Wow. The east coast ocean is very warm up through New Jersey. I can see this storm expanding and deepening as it comes up the coast.
I wonder if the canadian fires had something to do with the New England’s year without summer (snow flurries in July, crop failure, etc.). Here in Pittsburgh the sun is totally blotted out right now. Temps are struggling to make it to the 70 degree mark.
I believe you are correct. I totally forgot about that. Thanks for correcting me.
beautiful pict;ure of that thunderstorm
Henry, why is Pittsburgh (and Indiana, PA) a desert for t’storms. Is it the upward slope from Ohio to PA the problem. I thought we missed out on t’storms in Norristown but this is strange. BTW, Greg Zygmont says HI.
Can you explain a) how a closed low forms b) general description c) weather associated
A closed low develops when cold air aloft because detached from the main jet stream. Typically, you have a storm that becomes stacked under the upper level low but as the upper low matures, the weather goes from a storm to showery activity as the airmass becomes unstable under the cold pool or air aloft. We are now into a matured upper low that is…Read More
