CIMS Measurements of HNO sub(3) and SO sub(2) at the South Pole During ISCAT 2000

• Published in: Atmospheric environment (1994) 2004-10, Vol.38 (32), p.5411-5411
• Main Authors: Huey, L G, Tanner, D J, Slusher, D L, Dibb, JE, Arimoto, R, Chen, G, Davis, D
• Format: Article
• Language: English
• ISSN: 1352-2310
• DOI: 10.1016/j.atmosenv.2004.04.037

HNO sub(3) and SO sub(2) were measured by chemical ionization mass spectrometry at the South Pole (SP) during ISCAT 2000 (December, 2000). HNO sub(3) mixing ratios averaged 22 pptv and ranged from less than 5 to 68 pptv. A simple steady state photochemical analysis indicates that most of the time HNO sub(3) is deposited to the snow with a lifetime of the order of a few hours. Periods of relatively high levels of HNO sub(3) and low levels of NO were observed when air from aloft was mixed downward, but the source of this HNO sub(3) is uncertain. One explanation for these observations is that free tropospheric air, enriched with NO sub(x) at lower latitudes, descends to the surface at SP; this process could be an important source of nitrate to the Antarctic Plateau. Another explanation is that these descending air parcels were previously in contact with the surface and enriched with snowpack emissions of NO sub(x) upwind of SP. The measured SO sub(2) mixing ratio was found to be less than 20 pptv on average. However, a simple steady state analysis of OH and H sub(2)SO sub(4) observations indicates that average SO sub(2) levels are most likely less than a few pptv.