Sökning: WFRF:(Höpfner M.) > Höpfner M. > Piccolo C. > Bernath P. F. > Catoire V. > Toohey M. > Notholt J. > Teknik > Validation of NO2 a...
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000 | 06167naa a2201141 4500 | |
001 | oai:research.chalmers.se:993bb992-cd50-4a4a-85fd-06d2f2ed68f2 | |
003 | SwePub | |
008 | 171007s2008 | |||||||||||000 ||eng| | |
024 | 7 | a https://research.chalmers.se/publication/771362 URI |
024 | 7 | a https://doi.org/10.5194/acp-8-5801-20082 DOI |
040 | a (SwePub)cth | |
041 | a engb eng | |
042 | 9 SwePub | |
072 | 7 | a art2 swepub-publicationtype |
072 | 7 | a ref2 swepub-contenttype |
100 | 1 | a Kerzenmacher, T.4 aut |
245 | 1 0 | a Validation of NO2 and NO from the Atmospheric Chemistry Experiment (ACE) |
264 | c 2008-10-08 | |
264 | 1 | b Copernicus GmbH,c 2008 |
338 | a electronic2 rdacarrier | |
520 | a Vertical profiles of NO2 and NO have been obtained from solar occultation measurements by the Atmospheric Chemistry Experiment (ACE), using an infrared Fourier Transform Spectrometer (ACE-FTS) and (for NO2) an ultraviolet-visible-near-infrared spectrometer, MAESTRO (Measurement of Aerosol Extinction in the Stratosphere and Troposphere Retrieved by Occultation). In this paper, the quality of the ACE-FTS version 2.2 NO2 and NO and the MAESTRO version 1.2 NO2 data are assessed using other solar occultation measurements (HALOE, SAGE II, SAGE III, POAM III, SCIAMACHY), stellar occultation measurements (GOMOS), limb measurements (MIPAS, OSIRIS), nadir measurements (SCIAMACHY), balloon-borne measurements (SPIRALE, SAOZ) and ground-based measurements (UV-VIS, FTIR). Time differences between the comparison measurements were reduced using either a tight coincidence criterion, or where possible, chemical box models. ACE-FTS NO2 and NO and the MAESTRO NO2 are generally consistent with the correlative data. The ACE-FTS and MAESTRO NO2 volume mixing ratio (VMR) profiles agree with the profiles from other satellite data sets to within about 20% between 25 and 40 km, with the exception of MIPAS ESA (for ACE-FTS) and SAGE II (for ACE-FTS (sunrise) and MAESTRO) and suggest a negative bias between 23 and 40 km of about 10%. MAESTRO reports larger VMR values than the ACE-FTS. In comparisons with HALOE, ACE-FTS NO VMRs typically (on average) agree to ±8% from 22 to 64 km and to +10% from 93 to 105 km, with maxima of 21% and 36%, respectively. Partial column comparisons for NO2 show that there is quite good agreement between the ACE instruments and the FTIRs, with a mean difference of +7.3% for ACE-FTS and +12.8% for MAESTRO. | |
650 | 7 | a TEKNIK OCH TEKNOLOGIERx Maskinteknikx Rymd- och flygteknik0 (SwePub)203022 hsv//swe |
650 | 7 | a ENGINEERING AND TECHNOLOGYx Mechanical Engineeringx Aerospace Engineering0 (SwePub)203022 hsv//eng |
650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Meteorologi och atmosfärforskning0 (SwePub)105082 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Meteorology and Atmospheric Sciences0 (SwePub)105082 hsv//eng |
650 | 7 | a TEKNIK OCH TEKNOLOGIERx Annan teknikx Övrig annan teknik0 (SwePub)211992 hsv//swe |
650 | 7 | a ENGINEERING AND TECHNOLOGYx Other Engineering and Technologiesx Other Engineering and Technologies not elsewhere specified0 (SwePub)211992 hsv//eng |
650 | 7 | a TEKNIK OCH TEKNOLOGIERx Naturresursteknikx Annan naturresursteknik0 (SwePub)207992 hsv//swe |
650 | 7 | a ENGINEERING AND TECHNOLOGYx Environmental Engineeringx Other Environmental Engineering0 (SwePub)207992 hsv//eng |
653 | a NO2 | |
653 | a Satellite | |
653 | a Atmosphere | |
653 | a ACE | |
653 | a Validation | |
653 | a NO | |
700 | 1 | a Wolff, M.A.4 aut |
700 | 1 | a Strong, K.4 aut |
700 | 1 | a Dupuy, E.4 aut |
700 | 1 | a Walker, K.A.4 aut |
700 | 1 | a Amekudzi, L. K.4 aut |
700 | 1 | a Batchelor, R. L.4 aut |
700 | 1 | a Bernath, P.F.4 aut |
700 | 1 | a Berthet, G.4 aut |
700 | 1 | a Blumenstock, T.4 aut |
700 | 1 | a Boone, C.D.4 aut |
700 | 1 | a Bramstedt, K.4 aut |
700 | 1 | a Brogniez, C.4 aut |
700 | 1 | a Brohede, Samuel,d 1977u Chalmers tekniska högskola,Chalmers University of Technology4 aut0 (Swepub:cth)brohede |
700 | 1 | a Burrows, J. P.4 aut |
700 | 1 | a Catoire, V.4 aut |
700 | 1 | a Dodion, J.4 aut |
700 | 1 | a Drummond, J. R.4 aut |
700 | 1 | a Dufour, D. G.4 aut |
700 | 1 | a Funke, B.4 aut |
700 | 1 | a Fussen, D.4 aut |
700 | 1 | a Goutail, F.4 aut |
700 | 1 | a Griffith, D.W.T.4 aut |
700 | 1 | a Haley, C. S.4 aut |
700 | 1 | a Hendrick, F.4 aut |
700 | 1 | a Höpfner, M.4 aut |
700 | 1 | a Huret, N.4 aut |
700 | 1 | a Jones, N.4 aut |
700 | 1 | a Kar, J.4 aut |
700 | 1 | a Kramer, I.4 aut |
700 | 1 | a Llewellyn, E. J.4 aut |
700 | 1 | a Lopez-Puertas, M.4 aut |
700 | 1 | a Manney, G.4 aut |
700 | 1 | a McElroy, C.T.4 aut |
700 | 1 | a McLinden, C. A.4 aut |
700 | 1 | a Melo, S.4 aut |
700 | 1 | a Mikuteit, S.4 aut |
700 | 1 | a Murtagh, Donal,d 1959u Chalmers tekniska högskola,Chalmers University of Technology4 aut0 (Swepub:cth)donal |
700 | 1 | a Nichitiu, F.4 aut |
700 | 1 | a Notholt, J.4 aut |
700 | 1 | a Nowlan, C.4 aut |
700 | 1 | a Piccolo, C.4 aut |
700 | 1 | a Pommereau, J.P.4 aut |
700 | 1 | a Randall, C.4 aut |
700 | 1 | a Raspollini, P.4 aut |
700 | 1 | a Ridolfi, M.4 aut |
700 | 1 | a Richter, A.4 aut |
700 | 1 | a Schneider, M.4 aut |
700 | 1 | a Schrems, O.4 aut |
700 | 1 | a Silicani, M.4 aut |
700 | 1 | a Stiller, G. P.4 aut |
700 | 1 | a Taylor, J.4 aut |
700 | 1 | a Tétard, C.4 aut |
700 | 1 | a Toohey, M.4 aut |
700 | 1 | a Vanhellemont, F.4 aut |
700 | 1 | a Warneke, T.4 aut |
700 | 1 | a Zawodny, J.M.4 aut |
700 | 1 | a Zou, J.4 aut |
710 | 2 | a Chalmers tekniska högskola4 org |
773 | 0 | t Atmospheric Chemistry and Physicsd : Copernicus GmbHg 8:19, s. 5801--5841-q 8:19<5801--5841-x 1680-7316x 1680-7324 |
856 | 4 | u http://publications.lib.chalmers.se/records/fulltext/local_77136.pdfx primaryx freey FULLTEXT |
856 | 4 | u https://www.atmos-chem-phys.net/8/5801/2008/acp-8-5801-2008.pdf |
856 | 4 8 | u https://research.chalmers.se/publication/77136 |
856 | 4 8 | u https://doi.org/10.5194/acp-8-5801-2008 |
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