GROUND-BASED MICROWAVE MONITORING OF MIDDLE ATMOSPHERE OZONE - COMPARISON TO LIDAR AND STRATOSPHERIC AND GAS EXPERIMENT-II SATELLITE-OBSERVATIONS

被引:36
作者
TSOU, JJ
CONNOR, BJ
PARRISH, A
MCDERMID, IS
CHU, WP
机构
[1] JET PROPULS LAB, WRIGHTWOOD, CA 92397 USA
[2] UNIV MASSACHUSETTS, DEPT PHYS & ASTRON, AMHERST, MA 01003 USA
[3] LOCKHEED ENGN & SCI CO, HAMPTON, VA 23666 USA
[4] MILLITECH CORP, DEERFIELD, MA USA
关键词
D O I
10.1029/94JD02947
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A dedicated ground-based microwave radiometer was in operation to monitor the middle atmospheric ozone concentration at Table Mountain Facility (TMF) of the Jet Propulsion Laboratory (JPL), California (34.4 degrees N, 117.7 degrees W) from July 1989 to June 1992, as a part of the Network for Detection of Stratospheric Change. Ozone profiles from 56 to 0.04 mbar (similar to 20-70 km) were retrieved from the microwave data. The focus in this paper is to validate the microwave ozone observations from 56 to 1 mbar by comparing the results from a JPL ground-based lidar located at the same site and from the Stratospheric Aerosol and Gas Experiment II (SAGE II) satellite overpasses within 1000 km of TMF and to examine the ability of these instruments to detect short-term, seasonal, and annual variations in ozone. The profile comparison results show that the mean differences of microwave ozone from lidar and SAGE II are about 5% or less and the root-mean-square scatter about the mean is mainly from the precision of the instruments. A correlation analysis of ozone time series suggests highly significant correlations up to 2.4 mbar between lidar and microwave measurements and up to 1 mbar between SAGE II and microwave. The short-term and seasonal variation of the ozone profile seen in the microwave measurements is shown to be consistent with the observations of lidar and SAGE II, and the interannual variation of ozone appears to be detectable within an accuracy of a few percent with the microwave instrument.
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页码:3005 / 3016
页数:12
相关论文
共 31 条
[1]  
Barnett J. J., 1985, HDB MAP, V16, P47
[2]  
BRASSEUR G, 1984, COMPOSITION CHEM, P201
[3]   RADIO MEASUREMENT OF ATMOSPHERIC OZONE TRANSITION AT 101.7 GHZ [J].
CATON, WM ;
MANNELLA, GG ;
KALAGHAN, PM ;
BARRINGT.AE ;
EWEN, HI .
ASTROPHYSICAL JOURNAL, 1968, 151 (3P2) :L153-&
[4]  
CONNOR BJ, 1991, P SOC PHOTO-OPT INS, V1491, P218, DOI 10.1117/12.46665
[5]   OZONE OVER MCMURDO STATION, ANTARCTICA, AUSTRAL SPRING 1986 - ALTITUDE PROFILES FOR THE MIDDLE AND UPPER-STRATOSPHERE [J].
CONNOR, BJ ;
BARRETT, JW ;
PARRISH, A ;
SOLOMON, PM ;
DEZAFRA, RL ;
JARAMILLO, M .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D11) :13221-13230
[6]   GROUND-BASED MICROWAVE OBSERVATIONS OF OZONE IN THE UPPER-STRATOSPHERE AND MESOSPHERE [J].
CONNOR, BJ ;
SISKIND, DE ;
TSOU, JJ ;
PARRISH, A ;
REMSBERG, EE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D8) :16757-16770
[7]  
CONNOR BJ, 1995, IN PRESS J GEOPHYS R
[8]   VALIDATION OF SAGE-II OZONE MEASUREMENTS [J].
CUNNOLD, DM ;
CHU, WP ;
BARNES, RA ;
MCCORMICK, MP ;
VEIGA, RE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D6) :8447-8460
[9]   LARGE LOSSES OF TOTAL OZONE IN ANTARCTICA REVEAL SEASONAL CLOX/NOX INTERACTION [J].
FARMAN, JC ;
GARDINER, BG ;
SHANKLIN, JD .
NATURE, 1985, 315 (6016) :207-210
[10]  
FINGER FG, 1993, B AM METEOROL SOC, V74, P789, DOI 10.1175/1520-0477(1993)074<0789:EONUST>2.0.CO