If you are looking the qpf or simulated radar models this morning, you will notice the lack of t-storms today for the tri-state area. There a number of reasons why. First the NAM (as well as other models)show the core of 700-850mb jet streak over Northern parts of New England. On the left-rear side are westerly winds causing the air to dry and sink at the level, over the tri-state area. This will tend to suppress more thunderstorm development late this afternoon:
Models also show more instability, particularly CAPE over the Lower Mid-Atlantic region. Which is why the models like the NAM show more showers and thunderstorm forming along the cold front to the south of tri-state area. From experience, thunderstorm tend congregate in areas where more parameters, such as lift and instability are supportive. I still expect some showers and t-storms this afternoon. But over the tri-state area, there will be likely be more widely scattered with perhaps some isolated strong wind gusts. The chance of thunderstorms to reach severe levels are still very low. Latest guidance shows 0-6km shear increasing to 30kts to 40kts with a 50-60kt 500mb jet streak approach from north and west this afternoon. Which is not enough CAPE to support many tall or strong updrafts. Poor lapse rates and some cloud cover and onshore winds for the coast, will likely limit the amount of the instability this afternoon. As well reduce the ability for thunderstorms to produce damaging wind gusts. Pwats are still very high over 2.00″. So any thunderstorm is still capable of produce heavy rainfall and flash flooding poor drainage areas:







