© European Geosciences Union 2004
Abstract. We describe a sequential assimilation approach useful for assimilating tracer measurements into a threedimensional chemical transport model (CTM) of the stratosphere. The numerical code, developed largely according to Khattatov et al. (2000), uses parameterizations and simplifications allo...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.127.8172 2023-05-15T14:00:54+02:00 © European Geosciences Union 2004 B. Grassi G. Redaelli G. Visconti The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.127.8172 http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.127.8172 http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf text ftciteseerx 2016-01-07T14:22:55Z Abstract. We describe a sequential assimilation approach useful for assimilating tracer measurements into a threedimensional chemical transport model (CTM) of the stratosphere. The numerical code, developed largely according to Khattatov et al. (2000), uses parameterizations and simplifications allowing assimilation of sparse observations and the simultaneous evaluation of analysis errors, with reasonable computational requirements. Assimilation parameters are set by using χ 2 and OmF (Observation minus Forecast) statistics. The CTM used here is a high resolution threedimensional model. It includes a detailed chemical package and is driven by UKMO (United Kingdom Meteorological Office) analyses. We illustrate the method using assimilation of Upper Atmosphere Research Satellite/Microwave Limb Sounder (UARS/MLS) ozone observations for three weeks during the 1996 antarctic spring. The comparison of results from the simulations with TOMS (Total Ozone Mapping Spectrometer) measurements shows improved total ozone fields due to assimilation of MLS observations. Moreover, the assimilation gives indications on a possible model weakness in reproducing polar ozone values during springtime. Key words. Atmospheric composition and structure (middle atmosphere-composition and chemistry; instruments and techniques) 1 Text Antarc* Antarctic Unknown Antarctic |
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Abstract. We describe a sequential assimilation approach useful for assimilating tracer measurements into a threedimensional chemical transport model (CTM) of the stratosphere. The numerical code, developed largely according to Khattatov et al. (2000), uses parameterizations and simplifications allowing assimilation of sparse observations and the simultaneous evaluation of analysis errors, with reasonable computational requirements. Assimilation parameters are set by using χ 2 and OmF (Observation minus Forecast) statistics. The CTM used here is a high resolution threedimensional model. It includes a detailed chemical package and is driven by UKMO (United Kingdom Meteorological Office) analyses. We illustrate the method using assimilation of Upper Atmosphere Research Satellite/Microwave Limb Sounder (UARS/MLS) ozone observations for three weeks during the 1996 antarctic spring. The comparison of results from the simulations with TOMS (Total Ozone Mapping Spectrometer) measurements shows improved total ozone fields due to assimilation of MLS observations. Moreover, the assimilation gives indications on a possible model weakness in reproducing polar ozone values during springtime. Key words. Atmospheric composition and structure (middle atmosphere-composition and chemistry; instruments and techniques) 1 |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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B. Grassi G. Redaelli G. Visconti |
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B. Grassi G. Redaelli G. Visconti © European Geosciences Union 2004 |
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B. Grassi G. Redaelli G. Visconti |
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B. Grassi |
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© European Geosciences Union 2004 |
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© European Geosciences Union 2004 |
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© European Geosciences Union 2004 |
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© European Geosciences Union 2004 |
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© European Geosciences Union 2004 |
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© european geosciences union 2004 |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.127.8172 http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf |
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Antarc* Antarctic |
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Antarc* Antarctic |
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http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.127.8172 http://www.ann-geophys.net/22/2669/2004/angeo-22-2669-2004.pdf |
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