manner, situations characterized by similar local meteorological
features and initial basin conditions may be different in term of atmospheric circulation patterns
and therefore may lead to a different hydro-meteorological development and therefore differ-
ent streamflow scenarios in the following days. The use of synoptic information (method 4) is
therefore a complementary discriminating feature
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
that if two meteorological situations are similar regarding large
scale atmospheric circulation, they should also be similar with respect to local meteorological
conditions. Local meteorological conditions depend on the synoptic situation but local features
such as orography and surface properties play also an important role.
Considering a given meteorological situation characterised by some synoptic
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf