| Summary: | Individual measurements have been obtained from flask air samples returned to the CSIRO GASLAB. Typical sample storage times range from days to weeks for some sites (e.g. Cape Grim) to as much as 1 year for Macquarie Island and the Antarctic sites. Experiments carried out to test for changes in sample CO mixing ratio during storage have shown significant drifts in some flask types over test periods of several months to years (Cooper et al., 1999). Corrections derived from the test results are applied to network data according to flask type. (Data from the S160 flasks have been rejected due to large and variable drift.) An annual cycle of CO is evident, largely due to an increase in its destruction by the OH radical during the summer months. Additional influences include spatial and seasonal differences in source strength associated with varying trajectories of arriving air at different times of the year. Annual average CO mixing ratios at Alert in 2001 had decreased by about 13 percent of their 1993 value. A string of abnormally high monthly mixing ratios during the winter of 1998-1999, coupled with higher than normal mixing ratios during the previous summer, led to an anomalously high annual average for 1998. Elevated CO mixing ratios were observed on a global scale during 1998 (see Langenfelds et al., 2002).
|
|---|