T. Shibata et al., ARCTIC TROPOSPHERIC AEROSOLS AND CLOUDS IN THE POLAR NIGHT SEASON OBSERVED BY A LIDAR AT EUREKA, CANADA, Journal of Geomagnetism and Geoelectricity, 48(9), 1996, pp. 1169-1177
Vertical profiles of tropospheric aerosols and clouds were observed wi
th a lidar at Eureka (80 degrees N, 86 degrees W) in the Canadian high
Arctic. The observation periods were February, March and December 199
3, and January and February 1994. Observations were also performed fro
m December 1994 to March 1995. Vertical distributions of aerosols and
cloud particles are not easy to observe in the Arctic region especiall
y in the polar night season. The lidar observations showed us the firs
t overviews of Arctic tropospheric particle characteristics in mid-win
ter. Ice crystals were often observed, which correlate very well with
the relative humidity over ice that was observed by routine meteorolog
ical observations by radiosonde. Particle layers in a very dry environ
ment were sometimes observed.