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LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00006478naa a2200589 4500
001oai:DiVA.org:ltu-10938
003SwePub
008160929s2012 | |||||||||||000 ||eng|
009oai:research.chalmers.se:20c67055-f8e7-4a74-8f9a-db1c47056c04
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-109382 URI
0247 a https://doi.org/10.5194/amt-5-2809-20122 DOI
0247 a https://research.chalmers.se/publication/1669772 URI
040 a (SwePub)ltud (SwePub)cth
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Sato, T.O.u Tokyo Institute of Technology, 4259 Nagatsuta-cho, Midori-ku, Yokohama,Japan National Institute of Information and Communications Technology (NICT),National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei4 aut
2451 0a Strato-mesospheric ClO observations by SMILES :b error analysis and diurnal variation
264 c 2012-11-20
264 1b Copernicus GmbH,c 2012
338 a print2 rdacarrier
500 a Validerad; 2013; 20130103 (andbra)
520 a Chlorine monoxide (ClO) is the key species for anthropogenic ozone losses in the middle atmosphere. We observed ClO diurnal variations using the Superconducting Submillimeter-Wave Limb-Emission Sounder (SMILES) on the International Space Station, which has a non-sun-synchronous orbit. This includes the first global observations of the ClO diurnal variation from the stratosphere up to the mesosphere. The observation of mesospheric ClO was possible due to 10–20 times better signal-to-noise (S/N) ratio of the spectra than those of past or ongoing microwave/submillimeter-wave limb-emission sounders. We performed a quantitative error analysis for the strato- and mesospheric ClO from the Level-2 research (L2r) product version 2.1.5 taking into account all possible contributions of errors, i.e. errors due to spectrum noise, smoothing, and uncertainties in radiative transfer model and instrument functions. The SMILES L2r v2.1.5 ClO data are useful over the range from 0.01 and 100 hPa with a total error estimate of 10–30 pptv (about 10%) with averaging 100 profiles. The SMILES ClO vertical resolution is 3–5 km and 5–8 km for the stratosphere and mesosphere, respectively. The SMILES observations reproduced the diurnal variation of stratospheric ClO, with peak values at midday, observed previously by the Microwave Limb Sounder on the Upper Atmosphere Research Satellite (UARS/MLS). Mesospheric ClO demonstrated an opposite diurnal behavior, with nighttime values being larger than daytime values. A ClO enhancement of about 100 pptv was observed at 0.02 to 0.01 hPa (about 70–80 km) for 50° N–65° N from January–February 2010. The performance of SMILES ClO observations opens up new opportunities to investigate ClO up to the mesopause.
650 7a TEKNIK OCH TEKNOLOGIERx Maskinteknikx Rymd- och flygteknik0 (SwePub)203022 hsv//swe
650 7a ENGINEERING AND TECHNOLOGYx Mechanical Engineeringx Aerospace Engineering0 (SwePub)203022 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Meteorologi och atmosfärforskning0 (SwePub)105082 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Meteorology and Atmospheric Sciences0 (SwePub)105082 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Klimatforskning0 (SwePub)105012 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Climate Research0 (SwePub)105012 hsv//eng
653 a Space Technology
653 a Rymdteknik
7001 a Sagawa, H.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei,Japan National Institute of Information and Communications Technology (NICT)4 aut
7001 a Kreyling, D.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei,Japan National Institute of Information and Communications Technology (NICT)4 aut
7001 a Manabe, T.u Osaka Prefecture University, Naka, Sakai4 aut
7001 a Ochiai, S.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei4 aut
7001 a Kikuchi, K.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei,Japan National Institute of Information and Communications Technology (NICT)4 aut
7001 a Baron, P.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei,Japan National Institute of Information and Communications Technology (NICT)4 aut
7001 a Mendrok, Janau Luleå tekniska universitet,Rymdteknik,Luleå tekniska universitet (LTU),Luleå University of Technology (LTU),Japan National Institute of Information and Communications Technology (NICT)4 aut0 (Swepub:ltu)janmen
7001 a Urban, Joachim,d 1964u Chalmers University of Technology, Department of Earth and Space Sciences,Chalmers tekniska högskola4 aut0 (Swepub:cth)joaurb
7001 a Murtagh, Donal,d 1959u Chalmers University of Technology, Department of Earth and Space Sciences,Chalmers tekniska högskola4 aut0 (Swepub:cth)donal
7001 a Yasui, M.u National Institute of Information and Communications Technology, 4-2-1 Nukui-kitamachi, Koganei,Japan National Institute of Information and Communications Technology (NICT)4 aut
7001 a Kasai, Y.u Tokyo Institute of Technology, 4259 Nagatsuta-cho, Midori-ku, Yokohama,Japan National Institute of Information and Communications Technology (NICT)4 aut
7102 a Tokyo Institute of Technology, 4259 Nagatsuta-cho, Midori-ku, Yokohamab Tokyo Institute of Technology4 org
7730 t Atmospheric Measurement Techniquesd : Copernicus GmbHg 5:11, s. 2809-2825q 5:11<2809-2825x 1867-1381x 1867-8548
8564 u https://www.atmos-meas-tech.net/5/2809/2012/amt-5-2809-2012.pdf
8564 u http://publications.lib.chalmers.se/records/fulltext/166977/local_166977.pdfx primaryx freey FULLTEXT
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-10938
8564 8u https://doi.org/10.5194/amt-5-2809-2012
8564 8u https://research.chalmers.se/publication/166977

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