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IMK/IAA MIPAS temperature retrieval version 8: Nominal measurements

Authors :
Ministerio de Economía y Competitividad (España)
European Commission
Ministerio de Ciencia, Innovación y Universidades (España)
National Science Foundation (US)
Kiefer, Michael
von Clarmann, Thomas
Funke, Bernd
García Comas, Maia
Glatthor, Norbert
Grabowski, Udo
Kellmann, Sylvia
Kleinert, Anne
Laeng, Alexandra
Linden, Andrea
López-Puertas, Manuel
Marsh, Daniel R.
Stiller, Gabriele P.
Ministerio de Economía y Competitividad (España)
European Commission
Ministerio de Ciencia, Innovación y Universidades (España)
National Science Foundation (US)
Kiefer, Michael
von Clarmann, Thomas
Funke, Bernd
García Comas, Maia
Glatthor, Norbert
Grabowski, Udo
Kellmann, Sylvia
Kleinert, Anne
Laeng, Alexandra
Linden, Andrea
López-Puertas, Manuel
Marsh, Daniel R.
Stiller, Gabriele P.
Publication Year :
2021

Abstract

A new global set of atmospheric temperature profiles is retrieved from recalibrated radiance spectra recorded with the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS). Changes with respect to previous data versions include a new radiometric calibration considering the time dependency of the detector nonlinearity and a more robust frequency calibration scheme. Temperature is retrieved using a smoothing constraint, while tangent altitude pointing information is constrained using optimal estimation. ECMWF ERA-Interim is used as a priori temperature below 43 km. Above, a priori data are based on data from the Whole Atmosphere Community Climate Model Version 4 (WACCM4). Bias-corrected fields from specified dynamics runs, sampled at the MIPAS times and locations, are used, blended with ERA-Interim between 43 and 53 km. Horizontal variability of temperature is considered by scaling an a priori 3D temperature field in the orbit plane in a way that the horizontal structure is provided by the a priori while the vertical structure comes from the measurements. Additional microwindows with better sensitivity at higher altitudes are used. The background continuum is jointly fitted with the target parameters up to 58 km altitude. The radiance offset correction is strongly regularized towards an empirically determined vertical offset profile. In order to avoid the propagation of uncertainties of O3 and H2O a priori assumptions, the abundances of these species are retrieved jointly with temperature. The retrieval is based on HITRAN 2016 spectroscopic data, with a few amendments. Temperature-adjusted climatologies of vibrational populations of CO2 states emitting in the 15 µm region are used in the radiative transfer modeling in order to account for non-local thermodynamic equilibrium. Numerical integration in the radiative transfer model is now performed at higher accuracy. The random component of the temperature uncertainty typically varies between 0.4 and 1 K, wi

Details

Database :
OAIster
Notes :
English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1286584392
Document Type :
Electronic Resource