Blowing snow is a frequent and significant winter weather event, and
there is currently a need for more observations and measurements of
blowing snow, especially in arctic and subarctic environments. This book
describes the development of two camera systems which measure the size
and velocity of blowing snow particles and the relative blowing snow
density profile near the snow surface. These systems were used, along
with standard meteorological instruments and optical particle counters,
during field campaigns at Franklin Bay, NWT, and at Churchill, MB,
Canada. Results of these measurements are presented, which provide
valuable insight into the structure and dynamics of blowing snow.
Modelling studies with the Canadian Land Surface Scheme (CLASS) and
previous measurements of snow depth at Goose Bay, Hay River, the
Beaufort Sea, Franklin Bay, and Resolute demonstrate that blowing snow
sublimation can have a substantial effect on snow depth.