The results of correlated investigations of atmospheric carbon monoxid
e in Alaska during the spring-summer of 1995 using three different tec
hniques are presented. CO total column abundance was measured in Fairb
anks using IR spectroscopy with the Sun as a light source. A new compu
ter retrieval code was developed and compared with the previously used
technique. Surface mixing ratios were determined in situ by gas filte
r correlation and by gas chromatography with a mercuric oxide reductio
n detector. Surface measurements were made at two uncontaminated sites
: Poker Flat Research Range in interior Alaska and the National Oceani
c and Atmospheric Administration Point Barrow Observatory. In spring,
the measurements revealed considerably more CO in the surface layer as
compared with the tropospheric mean values determined by spectroscopy
. This suggests an accumulation of anthropogenic CO in the boundary at
mospheric layer over vast areas of the northern hemisphere during the
winter. Beginning in mid-April, the CO concentration in the tropospher
e decreases, but the rate of decrease in the surface layer was 2-2.5 t
imes greater than that for the troposphere as a whole. By June the sur
face mixing ratios and mean tropospheric values nearly converged, and
the CO mixing ratio seemed to be almost constant with altitude. The Ju
ly measurements revealed days with enhanced CO total column burden; th
ese are most likely associated with lifted layers of air, polluted by
forest fires.