Unsettled Northwest, Showers along cold front for Eastern States

By: Joe Roy @ 10:28 am March 19, 2009

joebanner2

The Pacific Northwest holds on to another cloudy day with mountain snows and valley showers as a frontal boundary is stalled offshore. The forecast doesn’t call for any improvement in the weather department as a stronger cold front will make it’s way onshore during the day Friday and bring with it an increased chance for valley rain and heavier mountain snows. The rest of the westcoast will get into the action later Saturday and through the day Sunday as a sharp upper-level trough really digs south through the  Westcoast States and into the desert Southwest.

The map below  illustrates where the cold front is currently situated (Coastal New England southwest to Northern Texas) and it’s associated cloudiness and anafrontal showers.

National Satellite/Radar Composite (13Z)

National Satellite/Radar Composite (13Z)

Showers along the cold front are generally light through New England and the Mid-Atlantic States. Heavier shower/t-storm activity may be found from Oklahoma to Tennessee where there are increased levels of instability.

Behind the cold front, northerly winds accompanied by a large area of high pressure building in from Canada will dry out the atmosphere under mostly sunny skies. Temperatures behind the front are running 10 to 20 degrees cooler today than this time yesterday across the Great Lakes and Mid-West.

The general pattern through the weekend will call for pleasant weather with a large ridge across the eastern third of the nation while the Western States will continue to be unsettled with below average temperatures, plenty of cloud cover, valley rain, and a lowering elevation for mountain snows.

2 Comments »

  • I was actually wondering why the showers and clouds were so far behind the cold front! I know that you can get some light instability behind a cold front certain times of the year and the occasional cumulus clouds and posibly a bit of precip.

    Do anafronts require higher temperature contrasts between the air masses to achieve stronger vertical development in the warm column?

    Vinnie

    Comment by Vincent Sapone — March 22, 2009 @ 8:36 am

  • Anafrontal precipitation takes place when a front advances faster than the flow in which it is embedded. The front advances due to wave propagation, and the flow responds accordingly. Warm air flows up the face of the frontal surface, which is typically not as steep as in a katafront (more often the case with cold fronts). The omega value are not as high (negative that is) and occurs over a larger surface area, generating an expanded precipitation shield.

    If memory serves me right, I dont believe the temperature contrast was that great along that front, good CAA followed pretty far behind it. If anything, in springtime when you see cold front’s with sharp horizontal temp gradients, their normally accompanied by squal lines and drier air right behind them.

    Joe

    Comment by Joe Roy — March 22, 2009 @ 12:49 pm

RSS feed for comments on this post. TrackBack URL

Leave a comment

© 2009-2012 4Cast4You All Rights Reserved