LOWER TROPOSPHERIC MEASUREMENTS OF HALOGENS, NITRATES, AND SULFUR-OXIDES DURING POLAR SUNRISE EXPERIMENT 1992

Citation
La. Barrie et al., LOWER TROPOSPHERIC MEASUREMENTS OF HALOGENS, NITRATES, AND SULFUR-OXIDES DURING POLAR SUNRISE EXPERIMENT 1992, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 99(D12), 1994, pp. 25453-25467
Citations number
23
Categorie Soggetti
Metereology & Atmospheric Sciences
Volume
99
Issue
D12
Year of publication
1994
Pages
25453 - 25467
Database
ISI
SICI code
Abstract
During the international Polar Sunrise Experiment 1992 at Alert, North west Territories, Canada, in the high Arctic, atmospheric chemistry me asurements were conducted from January to April to investigate lower t ropospheric ozone depletion chemistry. A series of filter-based measur ements involving a denuder and multistage filter holders were made to characterize the particulate and gaseous fraction of lower tropospheri c SOx, Br, Cl, I, and NO3- relation to O-3 depletion events. Bromine c ompounds were the only ones of all those measured to show correlations with ozone depletion. All three components of total Br (particulate i norganic, gaseous inorganic, and gaseous organic) increased during O-3 depletion events. Temporal trends in halogens between the dark of Jan uary and the complete light of April were in some cases evident. Large ly, as a result of more frequently occurring O-3 depletion-related epi sodes toward April, average concentrations of Br components tended to increase. The sum of inorganic particulate and gaseous Br increased fr om about 10 to 20 parts per trillion by volume (pptv) and organic gase ous Br increased from 25 to 40 pptv. Total inorganic I concentrations increased from about 0.3 pptv in early March to 1.0 pptv in late April . There was no systematic trend in total inorganic (gas plus particle) Cl with concentrations averaging approximately 40 pptv, while organic Cl trapped on charcoal was much more abundant. SOx concentrations ave raged about 1200 pptv, decreasing from a maximum of 6000 pptv in Janua ry to 800 pptv in April and were well correlated with anthropogenic V. The fraction of SOx oxidized to SO4= increased progressively from a l ow of 20 to 30% in January to greater than 80% in April. SO4= concentr ations increased from 500 pptv in January/February to 1000 pptv in Mar ch and dropped to 700 pptv in April. Inorganic NO3- showed no systemat ic variation throughout the period. It averaged 50 pptv, which is much less than peroxyacetyl nitrate (PAN) (150 to 600 pptv), and it was pr edominantly in particles. Judging from denuder observations, a filter combination of Teflon followed by two KOH filters can provide useful e stimates of inorganic particulate Br- and NO3- as well as of inorganic gaseous Br-. Inorganic gaseous NO3- measurements from KOH and nylon f ilters suffer interferences from collection of PAN.