GROUND-BASED AND AIRBORNE OBSERVATIONS OF CARBON-MONOXIDE DURING NASAMEASUREMENTS OF AIR-POLLUTION FROM SATELLITE (MAPS) MISSIONS SRL-1 AND SRL-2

Surface carbon monoxide (CO) data were acquired continuously at Heimae y, Iceland (63 degrees 24'N, 20 degrees 18'W), Mace Head, Ireland (53 degrees 19'N, 9 degrees 54'W), and Ragged Point, Barbados (13 degrees 15'N, 59 degrees 30'W), during April and October 1994, in support of M easurement of Air Pollution From Satellite (MAPS) Space Radar Laborato ry (SRL) missions SRL-1 and SRL-2, respectively, measuring middle trop ospheric CO from space. Observed median CO levels from the three surfa ce sites during these two MAPS missions approximate the monthly median for 1994 and are mostly typical of data from prior years. For two of the sites, computed mission isentropic back-trajectory ensemble probab ility fields are compared to seasonal (March-May and September-Novembe r) probability fields for 1994 and 1986-1995. Such comparisons help ga uge the representativeness of (1) observed surface air quality at, and (2) isentropic flow to, these sites during the mission periods, in te rms of intraseasonal and interannual variability. Results appear consi stent with longer-term flow climatological data and confirm the SRL-1 and SRL-2 mission periods are generally representative of the climatol ogy applicable to these sites for the time of year. Lower free troposp here in situ CO data were acquired from an aircraft over the Maryland Eastern Shore, on April 14 and October 3, 4, and 6. During the April f light a nearly linear gradient in CO with pressure from 1000-650 mbar of 225-150 parts per billion by volume (ppbv) was observed. At 650 mba r, CO was quite steady around 150 ppbv; this value compares favorably with the MAPS CO data for the closest 5 degrees x 5 degrees grid box a veraged April 13-15 of 105-120 ppbv. During SRL-2 a three flight CO av erage of 125 ppbv observed at similar to 725 mbar is in good agreement with the closest MAPS 5 degrees x 5 degrees grid box averaged October 3-7 of 90-105 ppbv. A layer of elevated CO at 845-740 mbar, most like ly the result of synoptic-scale transport, was observed during the Oct ober flights and seen to dissipate with time. The MAPS cloud-filtered second-by-second CO data during concurrent shuttle overflights show te mporal structure consistent with the in situ observations, indicating the MAPS weighting function may be capable of discerning features at l ower altitudes than thought previously.