Premium
Airborne measurements during the Arctic Stratospheric Experiment: Observation of O 3 and NO 2
Author(s) -
Pfeilsticker K.,
Platt U.
Publication year - 1994
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 - 10.1029/93gl01870
Subject(s) - differential optical absorption spectroscopy , environmental science , stratosphere , arctic , atmospheric sciences , ozone , aerosol , ozone depletion , the arctic , ozone layer , spectrometer , meteorology , total ozone mapping spectrometer , absorption (acoustics) , remote sensing , climatology , physics , optics , geology , oceanography
During winter 1991/92 DOAS (Differential Optical Absorption Spectroscopy) measurements were performed from a C130 Transall aircraft within the framework of the EASOE (European Arctic Stratospheric Ozone Experiment) campaign. The campaign extended from Dec. 1991 until March 1992 with a series of flights in the Arctic (60° W to 60° E , 85° N to 48° N ). Two spectrometers were operated on the aircraft: an UV‐instrument (see Brandtjen et al., this issue) and a DOAS‐vis instrument to detect O 3 , O 4 , NO 2 and NO 3 in the visible band (363 nm–680 nm). The DOAS‐vis ozone measurements were largely influenced by the presence of the Mt Pinatubo aerosol cloud. A correction of the data by actual Mie‐profiles is described. A NO 2 depletion with minimum values of 2.3*10 14 / cm ² in Jan. 92 was observed. Occasionally, OClO could also be detected.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom