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Measurements of nitrogen oxides in the Arctic
Author(s) -
Honrath R. E.,
Jaffe D. A.
Publication year - 1990
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl017i005p00611
Subject(s) - peroxyacetyl nitrate , noon , environmental science , sunrise , atmospheric sciences , reactive nitrogen , daytime , nitrogen dioxide , arctic , nitrate , nitrogen , meteorology , chemistry , nox , oceanography , geography , geology , organic chemistry , combustion
Nitric oxide (NO) and total reactive nitrogen (NO y ) were measured at the NOAA Geophysical Monitoring for Climatic Change baseline site near Barrow, Alaska, during July–August 1988. Concentrations of NO y in air from the clean‐air sector (45° to 130°) ranged from non‐detectable to 300 ppt (hourly‐average), with a median value of 100 ppt. NO concentrations were generally less than the detection limit of 50 ppt and reached a maximum of 100 ppt. These levels are similar to those observed at other remote sites, and are lower than the two previous measurements of NO y and peroxyacetyl nitrate (PAN) in the Arctic during spring. A diurnal cycle in NO y concentrations was also observed, with maximum levels near local solar noon, and minima near midnight. The cause of this cycle is not known, but it may be due to (1) daytime ventilation of NO y ‐rich air to the surface each day combined with fog scrubbing or dry deposition at night or (2) biological production of NO.