Seventeen horizontal aircraft passes were made across 0 degrees C regi
ons within 10 winter storms over Atlantic Canada. Regions of near free
zing temperatures (+/-1 degrees C) ranged from <2 km to 145 km in exte
nt. These regions were associated with both warm and cold fronts. The
detailed kinematic, thermodynamic and microphysical characteristics of
these regions were deduced Significant changes in these characteristi
cs often occur very close to 0 degrees C and indicate that these 0 deg
rees C regions were often directly associated with the locations of th
e fronts aloft. Microphysical processes involving phase changes of pre
cipitation significantly affect the nature of the atmosphere near thes
e 0 degrees C regions and in particular affect the structure of some o
f the fronts.