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Despite two disturbances, winter weather unlikely this weekend

In our previous article, we discussed some of the features in the upcoming hemispheric pattern that could support a winter weather event. These features were particularly evident during the period from January 16th to 20th. As we have gotten closer to this time period, forecast models have come into much better agreement on exactly how these features will evolve.

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Impressive Rain Storm 3/29 – 3/31

An impressive storm system is going to effect the Tri-State area this weekend into early Monday morning. The set-up in the upper atmosphere (500 mb) supports a long duration rain storm with frequent moderate to heavy rains which increases the flood threat, especially in areas where there is still snow / ice and if you live in a flood prone zone.

Timing:

Start: 12pm-1pm Saturday

End: 5am-7am Monday

This equates to 40+ hours of rain falling which when all is said and done could add up to 4+ inches of rain in some spots of the Northeast. Obviously the rain is not going to be heavy for 40+ hours. In fact, there may even be a brief break in the action before it starts up again. Nonetheless, we are still looking at a washout weekend with a potent coastal storm developing.

The 00z GFS 500 mb map by 2pm tomorrow is beginning to show a phase with the northern and southern stream energies in the atmosphere which will result in a strong surface low developing. By this time, rain is streaming up the coast into the northeast ahead of the surface low with the heaviest falling over Long Island.
Fast forward into early Sunday morning, and now those energies have completely phased with the H5 trough now closed off. At this time, very heavy rain is falling throughout NY state, the northern tier of PA, NNJ, and NYC into LI.
By Sunday night, the closed off low deepens with the H5 trough now going negative, prompting the coastal low to slow down and bring training moderate to heavy rainfall over parts of the coast from PA into NJ into NYC.
What is happening here is we are seeing the effects of Atlantic blocking and what it could do to east coast storms. Throughout this winter, we have been in a relatively zonal flow due to a constant +NAO with only a north-Atlantic ridge trying to help slow the flow down.
This time, the combination of positive heights into Greenland and eastern Canada have forced this storm to CUT-OFF from the jet stream and almost come to a stall off the coast of NJ. The good news is this will not be some 950 mb bomb of a storm that is bringing hurricane force winds to the area. It is expected to remain on the weak side with the worst of the winds along the immediate coast, where 30-40+ mph gusts can be expected.
RAIN MAP
Region wide, we are looking at 1.50-2.50 inches of rain for the most part. In further assessment, I can see how red-shaded areas receive possibly more than 3 inches of rain due to the positioning of the stalling low pressure storm off the coast of NJ. Some pieces of guidance support this notion of sending bands of rain over this area which would enhance rainfall totals. Obviously flooding in NNJ near the rivers could be a concern, but I do not believe rivers are in danger of flooding since it has been pretty dry of late. However, that does not mean roads that flood easily will not flood. So please keep that in mind.
Enjoy this miserable weekend,
Frank

 

Significant storm will bring rain, wind through Thursday

If you are a fan of changeable weather, today is for you. A major storm system, developing as a result of a mid level phase, will organize over the Tennessee Valley and shift northeastward to a position near New York City late tonight. The track will mean significant winter weather for our friends in Northern New England (including many of the major ski resorts), but more notably one of the more dramatic swings in sensible weather our area has seen in months. Temperatures will swing from the mid 60s to 70s in some spots this afternoon, all the way down into the 20s by Thursday morning.

Not surprisingly, the significant storm system moving through the Northeast US Wednesday into Thursday will feature a powerful thermal gradient and cold front. Initially, the thermal gradient will develop along a warm front which will stretch from southwest to northeast through the Northeast Wednesday afternoon. Parts of New Jersey could eclipse 70 degrees as southerly winds increase and temperatures increase in the low levels. Forecast models show drizzle and rain eventually increasing in coverage and intensity by Wednesday evening as moisture and lift begin to increase and the frontal boundary approaches Central Pennsylvania.

Regional radar imagery showing precipitation approaching the area (weather tap).

Regional radar imagery showing precipitation approaching the area as of 9:15am (weather tap).

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Widespread impacts from midweek storm

A pre-thanksgiving storm system will create a travel nightmare from Tuesday Night through Wednesday, providing a myriad of threats up and down the east coast. Before we dive into the details of the storm system, what’s causing it to occur, and what you can expect in our area, we can lay out a few things we know as fact as of Tuesday morning. First, there will be significant travel delays on Wednesday. If you’re driving, flying, or using some other form of travel in the Mid-Atlantic or Northeast US, expect delays…likely significant. Second, Thanksgiving day itself won’t be all that bad. So once you make it where you need to be, the weather for actual Turkey Day looks to be fairly pleasant, albeit a bit cold. In our post below, we break down the storm system and what you can expect from it.

Visible satellite imagery from Tuesday morning, showing a significant storm system forming in the Southeast US.

Visible satellite imagery from Tuesday morning, showing a significant storm system forming in the Southeast US.

What’s the deal, how is this storm forming?

Two pieces of energy in the jet stream across the Central and Eastern United States will phase on Wednesday, essentially very close to our forecast area. A low pressure area will develop from the Southeast States northeastward into New England. As it does so, warm air will stream up the Eastern Seaboard — as will significant amounts of precipitation in association with a strong low level jet and moisture transport. The low pressure system will then rapidly deepen as it moves to our north through New England and into Eastern Canada.

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