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Monday Mauler or Monday Bawler? part II


DDweatherman

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The dynamics are going to make or break this storm for SE areas. Models  have great upper level divergence, intense lift as shown on the 700 and 850 mb vv panels, and a ton of juice. That is what will produce the "cold enough" surface temps. If that doesnt work out wrt to alignment or timing, then its mostly heavy rain and sleet.

It is my experience that if you talk about a storm "producing" cold air... you get yelled at/ made fun of... but I think its possible.. or something like it (as described above).... 

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The dynamics are going to make or break this storm for SE areas. Models  have great upper level divergence, intense lift as shown on the 700 and 850 mb vv panels, and a ton of juice. That is what will produce the "cold enough" surface temps. If that doesnt work out wrt to alignment or timing, then its mostly heavy rain and sleet.

That's what I'm thinking also. We always hear how dynamics and rates overcome factors going against it. This will be a good test. I just hope the models are overdoing the QPF. but since their all on board with a lot of precip I guess it's a good bet

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Clouds and frozen river keeping DCA temps in check.. could be a saving grace

I am already at 50 near Navy Yard. Thought that was pretty high. Wouldn't be surprised to see it hit upper 50's. Clouds may help limit but will also limit cool down tonight before the rain starts.
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How do the dynamics set up as compared with jan 2011?  That was one of my favorite storms... it poured snow for about four hours... we gonna see anything like that?

I highly doubt we'll see anything of that magnitude around this time. We'll see some impressive dynamics with this storm, don't get me wrong, but the magnitude of that storm was incredible

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One of the things that has me a bit more optimistic about this storm is that at the low levels, flow is from the N and advecting in cold dry air (helps with evap cooling) - note that we did not have this on 3/6. The problems are at the mid levels where flow is more out of the WSW or even turns SW for a bit as the wave amplifies. So the key as many have mentioned is to get the strong upward motion to force moist adiabatic cooling. This is evident on the hires NAM output. This should be the type of storm where you go from heavy snow to drizzle depending on whether you are in a band or not, although a lot depends on how fast the cold air filters in. I'm guessing the rain/snow line will move S in jumps based on banding. Should be fun to watch although frustrating for those who miss out or change after wasting a lot of liquid on rain.

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