Blowing snow (snow transport) affects snow cover distribution and snow
melt runoff patterns in cold, wind-swept regions. This paper uses a st
atistical method to examine the occurrence of blowing snow and the met
eorological conditions recorded for 16 stations on the prairies of wes
tern Canada over six winters. The results show that the occurrence pro
bability is highly related to wind speed, air temperature and snow age
. For the same air temperature and snow age, the occurrence probabilit
y increases with increasing wind speed. The probability distribution o
f occurrence with respect to wind speed approximates a cumulative norm
al probability distribution, depending on the mean and variance of win
d speed: the location and scale parameters of the normal distribution.
It was found that these two statistical parameters essentially indica
te snow resistance and sensitivity to wind transport. Analysis of the
probability distributions for the occurrence of blowing snow for diffe
rent classes of air temperature and snow age reveals that the mean win
d speed of the normal distribution generally increases with increasing
air temperature and snow age, and the variance of wind speed increase
s with increasing air temperature. This leads to the development of a
model which first estimates the two parameters of the normal distribut
ion using air temperature and snow age, and then estimates the probabi
lity of the occurrence of blowing snow using wind speed and the two pa
rameters with the cumulative normal probability function. Comparison o
f hours of occurrence of blowing snow and of fluxes of snow transport
and sublimation estimated using the model to those determined using ob
servations of occurrence of blowing snow shows good agreement. The res
ults of this study can be used to estimate the frequency of blowing sn
ow events using standard meteorological data, to determine the snow tr
ansport and snow sublimation fluxes, and to examine the effect of mete
orological conditions on blowing snow processes.