http://www.osdpd.noaa.gov/PSB/EPS/SS...12.30.2006.gif

Trying to work out why the SST anomaly is so low close to Newfoundland
and Nova Scotia as it hasn't been cold in that region generally.
Forgetting the warm SST's above 50° Lat, it almost looks as though the
flow is further south. Also with a cooler pool to the south of 50° Lat,
the less steep gradient I should have though would produce much less
westerly mobility.

Still don't know what implications that massive cold pool in the NE
Pacific has?

Any thoughts, because the current weather pattern does not fit my line
of thought.
--
Keith (Southend)
http://www.southendweather.net
e-mail: kreh at southendweather dot net