A. Smirnov et al., AEROSOL OPTICAL DEPTH OVER CANADA AND THE LINK WITH SYNOPTIC AIR-MASSTYPES, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D14), 1996, pp. 19299-19318
Aerosol optical depth measurements acquired through the Canadian sunph
otometer network were statistically analyzed for the 1987-1992 period
in order to investigate spatial and temporal commonalities between the
member stations. Four stations were chosen to yield a spatially repre
sentative sampling of atmospheric optical conditions across Canada (Ea
st Coast, eastern continental, western continental, and West Coast), A
ll the stations were located in rural, local pollution free areas. The
results of aerosol optical depth measurements showed significant diff
erences between eastern and western Canadian stations. The effect of t
he Pinatubo volcanic eruption was clearly seen in the measurements acq
uired at Sable Island, Nova Scotia, Air mass relationships for the fou
r stations sampled demonstrated the relevance of applying air mass cla
ssification criteria to the analysis and discrimination of atmospheric
optical depth. Knowledge of the seasonal trend combined with informat
ion concerning air mass type enables a coarse a priori estimation of a
erosol optical depth in the absence of traditional optical data, Synop
tical air mass analysis facilitates the understanding of the mechanism
s involved in the seasonal variations of aerosol optical depth and yie
lds useful information about the atmospheric optical state, The releva
nce of the synoptical air mass approach was demonstrated in one partic
ular case: a seasonal aerosol optical depth trend for Arctic air masse
s was observed for the three sunphotometer stations which regularily e
xperience this type of air mass.