Validation of POAM III ozone:: Comparisons with ozonesonde and satellite data -: art. no. 4367

被引:70
作者
Randall, CE
Rusch, DW
Bevilacqua, RM
Hoppel, KW
Lumpe, JD
Shettle, E
Thompson, E
Deaver, L
Zawodny, J
Kyrö, E
Johnson, B
Kelder, H
Dorokhov, VM
König-Langlo, G
Gil, M
机构
[1] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80309 USA
[2] USN, Res Lab, Washington, DC 20375 USA
[3] Computat Phys Inc, Springfield, VA USA
[4] GATS Inc, Newport News, VA USA
[5] NASA, Langley Res Ctr, Hampton, VA 23665 USA
[6] Finnish Meteorol Inst, Spdankyla Observ, Sodankyla, Finland
[7] NOAA CMDL, Boulder, CO USA
[8] Royal Netherlands Meteorol Inst, KNMI, De Bilt, Netherlands
[9] Cent Aerol Observ, Moscow, Russia
[10] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany
[11] Inst Nacl Tecn Aeroespacial, LATMOS, Torrejon De Arroz, Spain
关键词
ozone; validation; POAM; solar occultation; SAGE; HALOE; HALOGEN OCCULTATION EXPERIMENT; STRATOSPHERIC AEROSOL; SAGE-II; POLAR OZONE; LOWERMOST STRATOSPHERE; UPPER TROPOSPHERE; ATMOS EXPERIMENT; PROFILES; VARIABILITY; INSTRUMENT;
D O I
10.1029/2002JD002944
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper describes the validation of ozone profiles from the Polar Ozone and Aerosol Measurement (POAM) III instrument. POAM III O-3 is measured with 1-km vertical resolution throughout most of the stratosphere and random errors of similar to5%. It is shown that sunspots do not significantly affect the POAM O-3 retrievals, nor do polar stratospheric clouds, except under rarely <LF>encountered, extreme conditions of very low O-3 and exceptionally high aerosol extinction. A statistical analysis is presented of comparisons between coincident measurements from POAM III and ozonesondes, the Halogen Occultation Experiment (HALOE) and the Stratospheric Aerosol and Gas Experiment (SAGE) II. On average, POAM III O-3 profiles agree to within +/-5% with these correlative data from 13 to 60 km. There is a suggestion that from 30 to 60 km POAM III sunrise data might be biased slightly low (<5%) relative to POAM sunset data. There is evidence that POAM III has a high bias of up to similar to 0.1 ppmv from 10 to 12 km, and that this bias might stem, in part, from errors in the retrieval of aerosol extinction at 0.6 mm, the primary O-3 absorption wavelength in the POAM retrievals. Below 10 km the POAM III data agree with coincident sonde measurements to better than 0.05 ppmv on average, which can correspond to large relative differences of more than +30% at 8-9 km and -100% at 5 km. We conclude that the POAM III profiles are highly accurate and adequate for quantitative scientific studies.
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页数:17
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