![CIMS measurements of HNO"3 and SO"2 at the South Pole during ISCAT 2000 [An article from: Atmospheric Environment]](https://www.ebooknetworking.net/books/B00/0RR/bigB000RR1FH8.jpg)
CIMS measurements of HNO"3 and SO"2 at the South Pole during ISCAT 2000 [An article from: Atmospheric Environment]
Description
This digital document is a journal article from Atmospheric Environment, published by Elsevier in 2004. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
HNO"3 and SO"2 were measured by chemical ionization mass spectrometry at the South Pole (SP) during ISCAT 2000 (December, 2000). HNO"3 mixing ratios averaged 22pptv and ranged from less than 5 to 68pptv. A simple steady state photochemical analysis indicates that most of the time HNO"3 is deposited to the snow with a lifetime of the order of a few hours. Periods of relatively high levels of HNO"3 and low levels of NO were observed when air from aloft was mixed downward, but the source of this HNO"3 is uncertain. One explanation for these observations is that free tropospheric air, enriched with NO"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"x upwind of SP. The measured SO"2 mixing ratio was found to be less than 20pptv on average. However, a simple steady state analysis of OH and H"2SO"4 observations indicates that average SO"2 levels are most likely less than a few pptv.
Description:
HNO"3 and SO"2 were measured by chemical ionization mass spectrometry at the South Pole (SP) during ISCAT 2000 (December, 2000). HNO"3 mixing ratios averaged 22pptv and ranged from less than 5 to 68pptv. A simple steady state photochemical analysis indicates that most of the time HNO"3 is deposited to the snow with a lifetime of the order of a few hours. Periods of relatively high levels of HNO"3 and low levels of NO were observed when air from aloft was mixed downward, but the source of this HNO"3 is uncertain. One explanation for these observations is that free tropospheric air, enriched with NO"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"x upwind of SP. The measured SO"2 mixing ratio was found to be less than 20pptv on average. However, a simple steady state analysis of OH and H"2SO"4 observations indicates that average SO"2 levels are most likely less than a few pptv.
