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Observations of the nitrate radical in the free troposphere at Izaña de Tenerife
Author(s) -
Carslaw Nicola,
Plane John M. C.,
Coe Hugh,
Cuevas Emilio
Publication year - 1997
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/96jd03512
Subject(s) - troposphere , differential optical absorption spectroscopy , atmospheric sciences , aerosol , altitude (triangle) , nitrate , environmental science , relative humidity , trace gas , planetary boundary layer , boundary layer , environmental chemistry , chemistry , meteorology , absorption (acoustics) , geology , materials science , physics , thermodynamics , organic chemistry , geometry , mathematics , composite material
This paper reports direct measurements of the nitrate radical (NO 3 ) in the lower free troposphere. The measurements were carried out at Izaña de Tenerife (2300 m altitude) in the Canary Islands during May 1994, using the technique of differential optical absorption spectroscopy (DOAS). The average nighttime NO 3 concentration in very clean air from the mid‐Atlantic was found to be 8 ppt, with a maximum observed concentration of about 20 ppt. Combining the NO 3 data with ancillary measurements of NO 2 and O 3 in a model shows that there are no important NO 3 scavengers in a part of the troposphere that is characterized by a very low relative humidity and aerosol particle count, and where the concentration of NO 2 is too small for significant quantities of N 2 O 5 to form. On occasion, the presence of a trace concentration of NO or an organic species such as α‐pinene is required to explain the observations. The lifetime of NO 3 at night was in excess of 2 hours, much longer than measured hitherto in the tropospheric boundary layer.

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