On 23/09/2013 22:40, Joe Egginton wrote:
On 23/09/2013 22:10, Graham wrote:
Low-level turbulent mixing caused by convection underneath the
subsidence
inversion is likely to be the main cause. When the cloud tops reach the
inversion they spread out resulting in a layer of stratocumulus.
Mostly found over Weston Coyney and Tideswell
Graham
And also Wolverhampton ! ;-)
And Cheltenham...
--
Paul Hyett, Cheltenham