Microwave observations and modeling of O-2((1)Delta(g)) and O-3 diurnal variation in the mesosphere

被引:22
作者
Sandor, BJ
Clancy, RT
Rusch, DW
Randall, CE
Eckman, RS
Siskind, DS
Muhleman, DO
机构
[1] SPACE SCI INST, BOULDER, CO 80303 USA
[2] NASA, LANGLEY RES CTR, DIV ATMOSPHER SCI, HAMPTON, VA 23681 USA
[3] CALTECH, DIV GEOL & PLANETARY SCI, PASADENA, CA 91125 USA
[4] UNIV COLORADO, LAB ATMOSPHER & SPACE PHYS, BOULDER, CO 80309 USA
[5] USN, RES LAB, WASHINGTON, DC 20375 USA
关键词
D O I
10.1029/96JD03585
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The first microwave measurements of an electronically excited molecular species in the Earth's atmosphere are presented. Local thermodynamic equilibrium (LTE) rotational line emission from mesospheric O-2((1) Delta(g)) was observed at a frequency of 255.01794 GHz (lambda similar to 1.2 mm), employing the National Radio Astronomy Observatory (NRAO) millimeter facility at Kitt Peak, Arizona (32 degrees N, 111 degrees W). The pressure-broadened line shapes of the O-2((1) Delta(g)) spectra, which were obtained in January and April 1992 and in January and November 1993, are inverted to retrieve O-2((1) Delta(g)) mixing profiles over the 50-70 km altitude region. The observed daytime abundances exceed ozone abundances in the lower mesosphere, which are separately retrieved with coincident O-3 spectral line (249.7886 GHz) observations. The January and November 1993 observations are binned into 20-60 min time intervals to study O-2((1) Delta(g)) diurnal behavior. Derived abundances of O-2((1) Delta(g)) between 50 and 70 km for the four observation dates are 9%, 31%, 3%, and 26%, respectively, each +/-10% higher than predicted, based on the simple photochemistry of lower mesospheric O-2((1) Delta(g)). Modeled variation of [O-2((1) Delta(g))] with time of day agrees with observed variation in that the observed difference between model and data abundances is constant throughout the daylight hours of each observation date. Model underprediction of [O-2((1) Delta(g))] is consistent with similar model underprediction of mesospheric [O-3]. A perturbation to the photochemical model that forces decreased ozone chemical loss brings brings both model [O-3] and [O-2((1) Delta(g))] into agreement with the observations. O-2((1) Delta(g)) abundances derived from these 1.2 mm observations agree with [O-2((1) Delta(g))] values derived from comparable SME observations of the 1.27 mu m emission, with assumption of a 3880 s O-2((1) Delta(g)) radiative lifetime [Badger et al., 1965]. The 6800 s O-2((1) Delta(g)) radiative lifetime proposed by Mlynczak and Nesbitt [1995] is ruled out by the similar comparison.
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页码:9013 / 9028
页数:16
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