Validation of stratospheric and mesospheric ozone observed by SMILES from International Space Station

被引：24

作者：

Kasai, Y. ^{[1
,2
]}

Sagawa, H. ^{[1
]}

Kreyling, D. ^{[1
]}

Dupuy, E. ^{[1
,3
]}

Baron, P. ^{[1
]}

Mendrok, J. ^{[1
,4
]}

Suzuki, K. ^{[1
,5
]}

Sato, T. O. ^{[1
,2
]}

Nishibori, T. ^{[1
,6
]}

Mizobuchi, S. ^{[6
]}

Kikuchi, K. ^{[1
]}

Manabe, T. ^{[7
]}

Ozeki, H. ^{[8
]}

Sugita, T. ^{[4
]}

Fujiwara, M. ^{[9
]}

Irimajiri, Y. ^{[1
]}

Walker, K. A. ^{[10
,11
]}

Bernath, P. F. ^{[12
]}

Boone, C. ^{[11
]}

Stiller, G. ^{[13
]}

von Clarmann, T. ^{[13
]}

Orphal, J. ^{[13
]}

Urban, J. ^{[14
]}

Murtagh, D. ^{[14
]}

Llewellyn, E. J. ^{[15
]}

Degenstein, D. ^{[15
]}

Bourassa, A. E. ^{[15
]}

Lloyd, N. D. ^{[15
]}

Froidevaux, L. ^{[16
]}

Birk, M. ^{[17
]}

Wagner, G. ^{[17
]}

Schreier, F. ^{[17
]}

Xu, J. ^{[17
]}

Vogt, P. ^{[17
]}

Trautmann, T. ^{[17
]}

Yasui, M. ^{[1
]}

机构：

[1] Natl Inst Informat & Commun Technol NICT, Koganei, Tokyo, Japan

[2] Tokyo Inst Technol, Yokohama, Kanagawa 227, Japan

[3] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan

[4] Lulea Univ Technol, Kiruna, Sweden

[5] Univ Tokyo, Grad Sch Arts & Sci, Meguro Ku, Tokyo, Japan

[6] Japan Aerosp Explorat Agcy JAXA, Tsukuba, Ibaraki, Japan

[7] Osaka Prefecture Univ, Naka Ku, Sakai, Osaka 591, Japan

[8] Toho Univ, Funabashi, Chiba 274, Japan

[9] Hokkaido Univ, Kita Ku, Sapporo, Hokkaido, Japan

[10] Univ Toronto, Toronto, ON, Canada

[11] Univ Waterloo, Waterloo, ON N2L 3G1, Canada

[12] Old Dominion Univ, Norfolk, VA USA

[13] Karlsruhe Inst Technol, Inst Meteorol & Climate Res IMK, D-76021 Karlsruhe, Germany

[14] Chalmers, S-41296 Gothenburg, Sweden

[15] Univ Saskatchewan, Inst Space & Atmospher Studies, Saskatoon, SK S7N 0W0, Canada

[16] CALTECH, Jet Prop Lab, Pasadena, CA USA

[17] German Aerosp Ctr DLR, Remote Sensing Technol Inst, Oberpfaffenhofen, Wessling, Germany

来源：

ATMOSPHERIC MEASUREMENT TECHNIQUES | 2013年 / 6卷 / 09期

基金：

美国国家航空航天局; 日本学术振兴会; 加拿大自然科学与工程研究理事会;

关键词：

ODIN/SMR LIMB OBSERVATIONS; MIPAS; RETRIEVAL; TEMPERATURE; PERFORMANCE; INSTRUMENT; PROFILES; MODE; HNO3; MLS;

D O I：

10.5194/amt-6-2311-2013

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

We observed ozone (O-3) in the vertical region between 250 and 0.0005 hPa (similar to 12-96 km) using the Superconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) on the Japanese Experiment Module (JEM) of the International Space Station (ISS) between 12 October 2009 and 21 April 2010. The new 4K superconducting heterodyne receiver technology of SMILES allowed us to obtain a one order of magnitude better signal-to-noise ratio for the O-3 line observation compared to past spaceborne microwave instruments. The non-sun-synchronous orbit of the ISS allowed us to observe O-3 at various local times. We assessed the quality of the vertical profiles of O-3 in the 100-0.001 hPa (similar to 16-90 km) region for the SMILES NICT Level 2 product version 2.1.5. The evaluation is based on four components: error analysis; internal comparisons of observations targeting three different instrumental setups for the same O-3 625.371 GHz transition; internal comparisons of two different retrieval algorithms; and external comparisons for various local times with ozonesonde, satellite and balloon observations (ENVISAT/MIPAS, SCISAT/ACE-FTS, Odin/OSIRIS, Odin/SMR, Aura/MLS, TELIS). SMILES O-3 data have an estimated absolute accuracy of better than 0.3 ppmv (3%) with a vertical resolution of 3-4 km over the 60 to 8 hPa range. The random error for a single measurement is better than the estimated systematic error, being less than 1, 2, and 7%, in the 40-1, 80-0.1, and 100-0.004 hPa pressure regions, respectively. SMILES O-3 abundance was 10-20% lower than all other satellite measurements at 8-0.1 hPa due to an error arising from uncertainties of the tangent point information and the gain calibration for the intensity of the spectrum. SMILES O-3 from observation frequency Band-B had better accuracy than that from Band-A. A two month period is required to accumulate measurements covering 24 h in local time of O-3 profile. However such a dataset can also contain variation due to dynamical, seasonal, and latitudinal effects.

引用

页码：2311 / 2338

页数：28

共 22 条

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