The sat. image below received at Plymouth Uni shows North Sea cloud
evaporating completely near NE England coast, and silhouetting the
East Anglian coast in partial dispersion.
Is this only a sea surface temperature phenomenon or could the onshore
winds be gradually affected by the changing synoptics which are
bringing southerlies and southwestelies aloft?
http://www4.plymouth.ac.uk/metnet/sa...T%20sample.jpg
Len
Wembury, SW Devon