Sökning: onr:"swepub:oai:DiVA.org:ltu-9448" > Validation of MIPAS...
Fältnamn | Indikatorer | Metadata |
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000 | 07390naa a2200625 4500 | |
001 | oai:DiVA.org:ltu-9448 | |
003 | SwePub | |
008 | 160929s2013 | |||||||||||000 ||eng| | |
024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-94482 URI |
024 | 7 | a https://doi.org/10.5194/acp-13-5791-20132 DOI |
040 | a (SwePub)ltu | |
041 | a engb eng | |
042 | 9 SwePub | |
072 | 7 | a ref2 swepub-contenttype |
072 | 7 | a art2 swepub-publicationtype |
100 | 1 | a Wetzel, G.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
245 | 1 0 | a Validation of MIPAS-ENVISAT H2O operational data collected between July 2002 and March 2004 |
264 | c 2013-06-14 | |
264 | 1 | b Copernicus GmbH,c 2013 |
338 | a print2 rdacarrier | |
500 | a Validerad; 2013; 20130812 (ysko) | |
520 | a Water vapour (H2O) is one of the operationally retrieved key species of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) instrument aboard the Environmental Satellite (ENVISAT) which was launched into its sun-synchronous orbit on 1 March 2002 and operated until April 2012. Within the MIPAS validation activities, independent observations from balloons, aircraft, satellites, and ground-based stations have been compared to European Space Agency (ESA) version 4.61 operational H2O data comprising the time period from July 2002 until March 2004 where MIPAS measured with full spectral resolution. No significant bias in the MIPAS H2O data is seen in the lower stratosphere (above the hygropause) between about 15 and 30 km. Differences of H2O quantities observed by MIPAS and the validation instruments are mostly well within the combined total errors in this altitude region. In the upper stratosphere (above about 30 km), a tendency towards a small positive bias (up to about 10 %) is present in the MIPAS data when compared to its balloon-borne counterpart MIPAS-B, to the satellite instruments HALOE (Halogen Occultation Experiment) and ACE-FTS (Atmospheric Chemistry Experiment, Fourier Transform Spectrometer), and to the millimeter-wave airborne sensor AMSOS (Airborne Microwave Stratospheric Observing System). In the mesosphere the situation is unclear due to the occurrence of different biases when comparing HALOE and ACE-FTS data. Pronounced deviations between MIPAS and the correlative instruments occur in the lowermost stratosphere and upper troposphere, a region where retrievals of H2O are most challenging. Altogether it can be concluded that MIPAS H2O profiles yield valuable information on the vertical distribution of H2O in the stratosphere with an overall accuracy of about 10 to 30% and a precision of typically 5 to 15% - well within the predicted error budget, showing that these global and continuous data are very valuable for scientific studies. However, in the region around the tropopause retrieved MIPAS H2O profiles are less reliable, suffering from a number of obstacles such as retrieval boundary and cloud effects, sharp vertical discontinuities, and frequent horizontal gradients in both temperature and H2O volume mixing ratio (VMR). Some profiles are characterized by retrieval instabilities. | |
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 |
653 | a Space Technology | |
653 | a Rymdteknik | |
700 | 1 | a Oelhaf, H.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
700 | 1 | a Berthet, G.u Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS, Orléans, France4 aut |
700 | 1 | a Bracher, A.u Institute of Environmental Physics and Remote Sensing (IUP/IFE), University of Bremen, Bremen, Germany4 aut |
700 | 1 | a Cornacchia, C.u CNR-IMAA, Consiglio Nazionale delle Ricerche – Istituto di Metodologie per l'Analisi Ambientale, Tito Scalo, Potenza, Italy4 aut |
700 | 1 | a Feist, D. G.u Max Planck Institute for Biogeochemistry, Jena, Germany4 aut |
700 | 1 | a Fischer, H.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
700 | 1 | a Fix, A.u Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany4 aut |
700 | 1 | a Iarlori, M.u CETEMPS – Dipartimento di Scienze Fisiche e Chimiche – Università degli Studi, L'Aquila, Italy4 aut |
700 | 1 | a Kleinert, A.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
700 | 1 | a Lengel, A.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
700 | 1 | a Milz, Mathiasu Luleå tekniska universitet,Rymdteknik4 aut0 (Swepub:ltu)mmilz |
700 | 1 | a Mona, L.u CNR-IMAA, Consiglio Nazionale delle Ricerche – Istituto di Metodologie per l'Analisi Ambientale, Tito Scalo, Potenza, Italy4 aut |
700 | 1 | a Müller, S. C.u Institute of Applied Physics (IAP), University of Bern, Bern, Switzerland4 aut |
700 | 1 | a Ovarlez, J.u Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS, Orléans, France4 aut |
700 | 1 | a Pappalardo, G.u CNR-IMAA, Consiglio Nazionale delle Ricerche – Istituto di Metodologie per l'Analisi Ambientale, Tito Scalo, Potenza, Italy4 aut |
700 | 1 | a Piccolo, C.u Istituto di Fisica Applicata "Nello Carrara" (IFAC), del Consiglio Nazionale delle Ricerche (CNR), Firenze, Italy4 aut |
700 | 1 | a Raspollini, P.u Istituto di Fisica Applicata "Nello Carrara" (IFAC), del Consiglio Nazionale delle Ricerche (CNR), Firenze, Italy4 aut |
700 | 1 | a Renard, J-Bu Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS, Orléans, France4 aut |
700 | 1 | a Rizi, V.u CETEMPS – Dipartimento di Scienze Fisiche e Chimiche – Università degli Studi, L'Aquila, Italy4 aut |
700 | 1 | a Rohs, S.u Institute for Energy and Climate Research – Stratosphere (IEK-7), Forschungszentrum Jülich, Jülich, Germany4 aut |
700 | 1 | a Schiller, C.u Institute for Energy and Climate Research – Stratosphere (IEK-7), Forschungszentrum Jülich, Jülich, Germany4 aut |
700 | 1 | a Stiller, G.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
700 | 1 | a Weber, M.u Institute of Environmental Physics and Remote Sensing (IUP/IFE), University of Bremen, Bremen, Germany4 aut |
700 | 1 | a Zhang, G.u Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany4 aut |
710 | 2 | a Institute for Meteorology and Climate Research (IMK), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germanyb Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS, Orléans, France4 org |
773 | 0 | t Atmospheric Chemistry And Physicsd : Copernicus GmbHg 13:11, s. 5791-5811q 13:11<5791-5811x 1680-7316x 1680-7324 |
856 | 4 | u https://www.atmos-chem-phys.net/13/5791/2013/acp-13-5791-2013.pdf |
856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-9448 |
856 | 4 8 | u https://doi.org/10.5194/acp-13-5791-2013 |
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