Precision improvements in the geo-fit retrieval of pressure and temperature from MIPAS limb observations by modeling CO2 line-mixing

Abstract In this paper, we present an improvement of the retrieval of pressure and temperature from the observations of the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) on board of the environmental satellite (ENVISAT). The improvement has been obtained by integrating a state-of-the-art CO2 line-mixing model in a two-dimensional inversion system (Geo-fit). We describe the implementation of this model in the Geo-fit system and we show its capability to reproduce the CO2 spectral features affected by line-mixing. The upgraded analysis algorithm provides a better fit of the set of MIPAS observations analyzed by the European Space Agency (ESA) ground segment although these observations have been selected with criteria that should avoid line-mixing effects. Moreover, we show that this set of observations can be extended improving the precision of the retrieved pressure and temperature fields without increasing the computing demands. Since the CO2 Q branches are very sensitive to pressure and temperature, the capability to model accurately the line-mixing effects opens the possibility to exploit at best these spectral regions to infer pressure and temperature distributions. According to this idea, we propose a new set of spectral intervals, including the most intense CO2 Q branches. It is shown that the analysis of these intervals provides a significant improvement (up to 70%) in the precision of the retrieved pressure and temperature profiles, while using a smaller number of observations with respect to the ESA ground segment analysis. Since the knowledge of pressure and temperature is necessary for the retrieval of the altitude distribution of all the atmospheric constituents, the benefits of more precise pressure and temperature fields obtained in this work propagate into the quality of all the MIPAS products.

[1]  C. Rinsland,et al.  Middle and upper atmosphere pressure-temperature profiles and the abundances of CO2 and CO in the upper atmosphere from ATMOS/Spacelab 3 observations , 1992 .

[2]  Laurence S. Rothman,et al.  The HITRAN molecular spectroscopic database: edition of 2000 including updates through 2001 , 2003 .

[3]  P. R. Bevington,et al.  Data Reduction and Error Analysis for the Physical Sciences , 1969 .

[4]  Jonathan P. Taylor,et al.  The ISSWG line-by-line inter-comparison experiment , 2003 .

[5]  Jean-Michel Hartmann,et al.  Spectra calculations in central and wing regions of CO , 2004 .

[6]  M. Kiefer,et al.  Retrieval of temperature and tangent altitude pointing from limb emission spectra recorded from space by the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) , 2003 .

[7]  J. Remedios,et al.  Colour indices for the detection and differentiation of cloud types in infra-red limb emission spectra , 2004 .

[8]  P. Rosenkranz Shape of the 5 mm oxygen band in the atmosphere , 1975 .

[9]  P. E. Morris,et al.  Fast monochromatic radiative transfer calculations for limb sounding , 2002 .

[10]  C. Rinsland,et al.  Pressure sounding of the middle atmosphere from ATMOS solar occultation measurements of atmospheric CO(2) absorption lines. , 1996, Applied optics.

[11]  P. E. Morris,et al.  Optimized forward model and retrieval scheme for MIPAS near-real-time data processing. , 2000, Applied optics.

[12]  Clive D Rodgers,et al.  Microwindow selection for high-spectral-resolution sounders. , 2002, Applied optics.

[13]  K. Jucks,et al.  Model, software, and database for computation of line-mixing effects in infrared Q branches of atmospheric CO2: II Minor and asymmetric isotopomers , 1999 .

[14]  S. Green Pressure broadening and line coupling in bending bands of CO2 , 1989 .

[15]  K. Jucks,et al.  Spectra calculations in central and wing regions of CO2 IR bands between 10 and 20 μm. III: atmospheric emission spectra , 2004 .

[16]  C. B. Farmer,et al.  Stratospheric and mesospheric pressure‐temperature profiles from rotational analysis of CO2 lines in atmospheric trace molecule spectroscopy/ATLAS 1 infrared solar occultation spectra , 1995 .

[17]  Larrabee L. Strow,et al.  An overview of the AIRS radiative transfer model , 2003, IEEE Trans. Geosci. Remote. Sens..

[18]  M Carlotti,et al.  Geo-fit Approach to the Analysis of Limb-Scanning Satellite Measurements. , 2001, Applied optics.

[19]  R. Gordon,et al.  Line Shapes in Molecular Spectra , 1968 .

[20]  A. Ben-Reuven Impact Broadening of Microwave Spectra , 1966 .

[21]  C. Boulet,et al.  Temperature dependence of the absorption in the region beyond the 4.3-microm band head of CO(2) . 2: N(2) and O(2) broadening. , 1985, Applied optics.

[22]  Bernd Funke,et al.  CO2 LINE MIXING IN MIPAS LIMB EMISSION SPECTRA AND ITS INFLUENCE ON RETRIEVAL OF ATMOSPHERIC PARAMETERS , 1998 .

[23]  F. Hase,et al.  Spectra calculations in central and wing regions of CO2 IR bands between 10 and 20 μm. II. Atmospheric solar occultation spectra , 2004 .

[24]  J. Susskind,et al.  Spectral band passes for a high precision satellite sounder. , 1977, Applied optics.

[25]  L. Larrabee Strow,et al.  Fast computation of monochromatic infrared atmospheric transmittances using compressed look-up tables , 1998 .

[26]  C. Rinsland,et al.  Stratospheric temperature profile from balloon-borne measurements of the 10.4-μm band of CO2 , 1983 .

[27]  Marco Ridolfi,et al.  MIPAS-ENVISAT limb-sounding measurements: trade-off study for improvement of horizontal resolution. , 2004, Applied optics.

[28]  M. Ridolfi,et al.  Multi-target retrieval (MTR): the simultaneous retrieval of pressure, temperature and volume mixing ratio profiles from limb-scanning atmospheric measurements , 2004 .

[29]  Marco Prevedelli,et al.  GMTR: two-dimensional geo-fit multitarget retrieval model for michelson interferometer for passive atmospheric sounding/environmental satellite observations. , 2006, Applied optics.

[30]  S. Hannon,et al.  A compilation of first-order line-mixing coefficients for CO2 Q-branches , 1994 .