Minor constituent concentrations measured from a high altitude aircraft using high resolution far-infrared Fourier Transform spectroscopy

被引:6
作者
Carli, B [1 ]
Ade, P
Carlotti, M
Cortesi, U
Gignoli, A
Hamilton, P
Lanfranchi, M
Lee, C
MacKenzie, AR
Phillips, A
机构
[1] CNR, Ist Ric Onde Elettromagnet, Firenze, Italy
[2] Univ London Queen Mary & Westfield Coll, Dept Phys, London E1 4NS, England
[3] Univ Bologna, Dipartimento Chim Fis & Inorgan, I-40126 Bologna, Italy
[4] Univ London Queen Mary & Westfield Coll, Dept Chem, London E1 4NS, England
[5] Univ Lancaster, Dept Environm Sci, Lancaster LA1 4YW, England
关键词
far-infrared emission spectroscopy; high altitude aircraft; minor atmospheric constituents; stratospheric ozone chemistry; airborne polar experiment;
D O I
10.1023/A:1006316026239
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Far-infrared emission spectroscopy has been demonstrated to be a valuable method for remote sensing of trace species in the stratosphere, with the ability to simultaneously detect a number of key chemical species. SAFIRE-A is a new far-infrared Fourier Transform (FT) spectrometer which has been specifically designed to operate on board of a high altitude aircraft in the lower stratosphere and upper troposphere regions where relatively few remote sensing measurements have been made. Using new technology, the sensitivity of the FT spectrometer method has been substantially improved for the long wavelength region. Results are reported for measurements of O-3, HNO3 and N2O at 17 and 19 km using a detection window near 23 cm(-1). Geographical and altitude variability of the volume mixing ratio of these constituents and their relative correlation are discussed. Ozone measurements agree well with in situ measurements, except in regions of strong stirring and mixing associated with deformation of the northern vortex edge. Whilst SAFIRE measurements of trace gases do not capture all of the local variability seen by rapid in-situ techniques, they can indicate horizontal variability close to, but not intercepted by, the aircraft's flight path. A possible detection of ClO at the low background levels expected outside the polar vortex is also reported.
引用
收藏
页码:273 / 293
页数:21
相关论文
共 42 条
[1]  
[Anonymous], 1976, US STANDARD ATMOSPHE
[2]  
BODEKER GE, 1997, P 4 EUR S SCHL GERM, P415
[3]  
BRASSEUR G, 1996, AERONOMY MIDDLE ATMO, V101, P10217
[4]  
Brasseur G., 1986, AERONOMY MIDDLE ATMO, DOI [10.1007/978-94-009-4762-7, DOI 10.1007/978-94-009-4762-7]
[5]   AIRCRAFT MEASUREMENTS OF O-3, HNO3 AND N2O IN THE WINTER ARCTIC LOWER STRATOSPHERE DURING THE STRATOSPHERE-TROPOSPHERE EXPERIMENT BY AIRCRAFT MEASUREMENTS (STREAM) .1. [J].
BREGMAN, A ;
VANVELTHOVEN, PFJ ;
WIENHOLD, FG ;
FISCHER, H ;
ZENKER, T ;
WAIBEL, A ;
FRENZEL, A ;
ARNOLD, F ;
HARRIS, GW ;
BOLDER, MJA ;
LELIEVELD, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D6) :11245-11260
[6]   THE MIXING-RATIO OF THE STRATOSPHERIC HYDROXYL RADICAL FROM FAR INFRARED-EMISSION MEASUREMENTS [J].
CARLI, B ;
CARLOTTI, M ;
DINELLI, BM ;
MENCARAGLIA, F ;
PARK, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D8) :11049-11058
[7]   SUBMILLIMETER HIGH-RESOLUTION FT SPECTROMETER FOR ATMOSPHERIC STUDIES [J].
CARLI, B ;
MENCARAGLIA, F ;
BONETTI, A .
APPLIED OPTICS, 1984, 23 (15) :2594-2603
[8]   SUBMILLIMETER MEASUREMENT OF STRATOSPHERIC CHLORINE MONOXIDE [J].
CARLI, B ;
MENCARAGLIA, F ;
CARLOTTI, M ;
DINELLI, BM ;
NOLT, I .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D6) :7063-7068
[9]  
CARLI B, 1999, IN PRESS J ATMOS OCE
[10]   GLOBAL-FIT APPROACH TO THE ANALYSIS OF LIMB-SCANNING ATMOSPHERIC MEASUREMENTS [J].
CARLOTTI, M .
APPLIED OPTICS, 1988, 27 (15) :3250-3254