2/12/12 A cold February day... Finally

Yesterdays missed winter storm only brought some light flurries to the area as the storm intensified to far south and east of Southern New England to bring any accumulating snows. In fact, one would have to travel to far northern and eastern Maine to see any significant snows where up to 5" fall.

Satellite image of yesterdays storm intensifying over Nova Scotia. Too far east to influence much of our weather.

 The storm though did bring in behind it a much colder arctic air mass this morning, with temperatures falling rapidly overnight with much of New England now in a deep freeze.

From the WxBears weather station, the Arctic front passed coastal MA at 10 PM last night bringing a rapid drop in temperatures to a morning low of 14.9F.

The coldest air will remain in Northern New England and Maine where temperatures will struggle to get above Zero in some areas.

 For Sunday, a strong Northwest Wind will continue to bring allow for some CAA (Cold Air Advection) from Canada and will only bring temperatures up to the mid and upper 20's with wind chill values in the single digits and teens today.

A dry week ahead, except for an overnight passing shower as a warm front pushes through Tuesday night

Technical Stuff!!!

 A meteorologist will use many weather maps, but one of the most helpful is what is called the 500mb chart.  This map is produced by launching weather balloons at the same time across the world to get a picture of what the flow of the atmosphere is like.


The map is useful in showing many details, including "waves" of weather which are known as troughs and ridges. 

• A trough, is a dip and signifies typically colder and negative (stormy) weather. Shown in a red line.   

• A ridge is an area of typically warmer and good weather. Shown in a blue zigzag. 

The map above is showing a very large trough that has dug down into the east coast. This trough is allowing cold air from Canada to dip deep into the south as indicated by the blue arrows.  When a meteorologist sees such a trough, they can expect a storm to form ahead of it.  

• In most cases in the weather, it is what happens above that influences the main surface weather.

The 500mb map typically lags the surface map, whereas on this map the trough is just about to enter New England, the surface storm has already developed.  And even though we are in the sunshine today, we must wait for the trough to either pass or modify in order to change the weather. 

 Think of this map as a roller coaster ride, and the blue arrows are cars full of cold air. The cars have just dived from Canada deep on the tracks into the South with cold air and are rounding the curve to climb back up. However, when they do this they are picking up moisture  and are full of energy to produce a storm.