AIRBORNE MEASUREMENTS OF TOTAL SULFUR GASES DURING NASA GLOBAL TROPOSPHERIC EXPERIMENT CHEMICAL INSTRUMENTATION TEST AND EVALUATION-3

A metal foil collection/flash desorption/flame photometric detection ( MFC/FD/FPD) technique was used by investigators from the University of Idaho (UI) to measure ambient total sulfur gas concentrations from an aircraft platform during the NASA Global Tropospheric Experiment/Chem ical Instrumentation Test and Evaluation 3 (GTE/CITE 3) program. The M FC/FD/FPD technique allowed rapid quantitation of tropospheric backgro und air masses using sample integration times of 1-3 min with little o r no gap between measurements. The rapid and continual sampling nature of this technique yielded data covering approximately 75% of the enti re CITE 3 program's air track. Ambient air measurement data obtained d uring northern hemisphere (NH) flights often exhibited relatively high total sulfur gas values (up to 19 ppb) and an extremely high degree o f sample heterogeneity, especially in coastal locations. Data from sou thern hemisphere (SH) flights typically exhibited relatively low total sulfur gas concentrations and a low degree of sample heterogeneity. A bimodal interhemispheric total sulfur gas gradient was observed using data obtained during transit flights between the two CITE 3 program g round bases. Comparisons were made of UI total sulfur gas measurements with composite sulfur gas values generated using speciated sulfur gas measurements from other CITE 3 participants. Only a relatively small number of overlap periods for comparison were obtained from all the av ailable CITE 3 data because of large differences in measurement integr ation times and lack of synchronization of sample start/stop times for the various investigators. These effects were compounded with extreme sample heterogeneity in the NH and the speed at which the aircraft tr aversed the air masses being sampled. Despite these constraints, suffi cient overlapping data were available for the comparative evaluations. Comparison of NH UI total with composite sulfur gas values showed exc ellent correlation and linear curve fit, indicating substantial qualit ative agreement. Simple linear regression of total on composite sulfur gas data yielded a slope of 1.9 for coastal NH regions and 1.2 for ma rine NH regions. The marine NH slope is not statistically different fr om one, indicating substantial quantitative agreement between UI total and composite sulfur gas values in these regions. However, a signific ant difference was observed when these same data were treated with a p aired t test. SH data exhibited no significant correlation or linear r egression slope. A paired t test showed a statistically significant di fference when all SH flights were used. However, data from three SK fl ights that were classified into a unique group using discriminant anal ysis showed no significant difference between UI total and composite s ulfur gas values when analyzed with the paired t test.