On Fri, 31 May 2013 17:31:48 +0100, Vidcapper
wrote:
Looks like the Arctic is still basking in a heatwave at the
moment, northern Scandinavia currently +28°C.
How did such warmth get up there?
Strong advection of warm air around the side of a persistent block,
and probably some descent at times leading to adiabatic compression.
--
Freddie
Bayston Hill
Shropshire
102m AMSL
http://www.hosiene.co.uk/weather/
https://twitter.com/#!/BaystonHillWx for hourly reports