The temperature dependence (203-293 K) of the absorption cross sections of O3 in the 230-850 nm region measured by Fourier-transform spectroscopy

被引:164
作者
Voigt, S
Orphal, J
Bogumil, K
Burrows, JP
机构
[1] Univ Bremen, Inst Umweltphys, D-28334 Bremen, Germany
[2] Univ Bremen, Inst Fernerkundung, D-28334 Bremen, Germany
关键词
ozone; atmospheric remote-sensing; photochemical modelling;
D O I
10.1016/S1010-6030(01)00480-4
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Absolute absorption cross sections of O-3 were measured in the 230-850 nm (11765-43478 cm(-1)) region at five different temperatures (203-293 K) using a Fourier-transform spectrometer, at a spectral resolution of 5.0 cm(-1) (corresponding to about 0.027 nm at 230 nm and to about 0.36 nm at 850 nm). The spectral accuracy of the data is better than 0.1 cm(-1) - about 0.5 pm at 230 nm and about 7.2 pm at 850 nm - validated by recording of I-2 absorption spectra in the visible using the same experimental set-up. O-3 absorption spectra at different concentrations were recorded at five different sample temperatures in the range 203-293 K, and at each temperature at two total pressures (100 and 1000 mbar) using O-2/N-2 mixtures as buffer gas. Within the limits of experimental uncertainties, no influence of total pressure on the O-3 spectrum was observed in the entire spectral region, as expected from the short lifetimes of the upper electronic states of O-3. The temperature dependence of the O-3 absorption cross sections is particularly strong in the Huggins bands between 310 and 380 nm, as observed in previous studies. An empirical formula is used to model the temperature dependence of the O-3 absorption cross sections between 236 and 362 nm, a spectral region that is particularly important for atmospheric remote-sensing and for photochemical modelling. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:1 / 9
页数:9
相关论文
共 75 条
[1]   ABSORPTION CROSS-SECTIONS OF OZONE IN THE 590-NM TO 610-NM REGION AT T = 230-K AND T = 299-K [J].
AMORUSO, A ;
CACCIANI, M ;
DISARRA, A ;
FIOCCO, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D12) :20565-20568
[2]   LASER MEASUREMENTS OF OZONE ABSORPTION CROSS-SECTIONS IN THE CHAPPUIS BAND [J].
ANDERSON, SM ;
MAUERSBERGER, K .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (09) :933-936
[3]  
[Anonymous], 1953, ANN PHYS, DOI DOI 10.1051/ANPHYS/195312080709
[4]  
BALLARD J, 1998, STUDY ABSORPTION CRO
[5]   TEMPERATURE-DEPENDENCE OF THE OZONE ABSORPTION CROSS-SECTION AT THE 2537-NM MERCURY LINE [J].
BARNES, J ;
MAUERSBERGER, K .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D12) :14861-14864
[6]  
Bass A.M., 1985, ATMOSPHERIC OZONE P, P606, DOI DOI 10.1007/978-94-009-5313-0_120
[7]   O 1D quantum yields from O3 photolysis in the near UV region between 305 and 375 nm [J].
Bauer, D ;
D'Ottone, L ;
Hynes, AJ .
PHYSICAL CHEMISTRY CHEMICAL PHYSICS, 2000, 2 (07) :1421-1424
[8]   The Wulf bands of oxygen [J].
Bernath, P ;
Carleer, M ;
Fally, S ;
Jenouvrier, A ;
Vandaele, AC ;
Hermans, C ;
Merienne, MF ;
Colin, R .
CHEMICAL PHYSICS LETTERS, 1998, 297 (3-4) :293-299
[9]   The calculation of the bound and quasibound vibrational states for ozone in its B-1(2) electronic state [J].
Bludsky, O ;
Jensen, P .
MOLECULAR PHYSICS, 1997, 91 (04) :653-661
[10]  
BOGUMIL K, 1999, P 1 EUR S ATM MEAS S, V2, P443