Abstract

Abstract. The information load (IL) analysis, first introduced for the two-dimensional approach (Carlotti and Magnani, 2009), is applied to the inversion of MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) observations operated with a 1-dimensional (1-D) retrieval algorithm. The IL distribution of MIPAS spectra is shown to be often asymmetrical with respect to the tangent points of the observations and permits us to define the preferential latitude where the profiles retrieved with a 1-D algorithm should be geo-located. Therefore, defining the geo-location of the retrieved profile by means of the tangent points leads to a "position error". We assess the amplitude of the position error for some of the MIPAS main products and we show that the IL analysis can also be used as a tool for the selection of spectral intervals that, when analyzed, minimize the position error of the retrieved profile. When the temperature (T) profiles are used for the retrieval of volume mixing ratio (VMR) of atmospheric constituents, the T-position error (of the order of 1.5 degrees of latitude) induces a VMR error that is directly connected with the horizontal T gradients. Temperature profiles can be externally-provided or determined in a previous step of the retrieval process. In the first case, the IL analysis shows that a meaningful fraction (often exceeding 50%) of the VMR error deriving from the 1-D approximation is to be attributed to the mismatch between the position assigned to the external T profile and the positions where T is required by the analyzed observations. In the second case the retrieved T values suffer by an error of 1.5–2 K due to neglecting the horizontal variability of T; however the error induced on VMRs is of minor concern because of the generally small mismatch between the IL distribution of the observations analyzed to retrieve T and those analyzed to retrieve the VMR target. An estimate of the contribution of the T-position error to the error budget is provided for MIPAS main products. This study shows that the information load analysis can be successfully exploited in a 1-D context that makes the assumption of horizontal homogeneity of the analyzed portion of atmosphere. The analysis that we propose can be extended to the 1-D inversion of other limb-sounding experiments.

Highlights

  • Hydrology andLimb-scanning measuremEenatsrthhavSe pyrsovteenmto be especially suited to study the chemical comSpcosieitinoncoefsthe atmosphere and to determine the vertical distribution of atmospheric constituents

  • In order to assess the propagation of the T -position error into volume mixing ratio (VMR) retrievals, we distinguish the case in which T profiles are of external origin from the case of T profiles determined in a previous step of the retrieval analysis

  • Presence of horizontal T gradients, the T -position error is expected to propagate into the retrieved VMR profiles

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Summary

Introduction

Limb-scanning measuremEenatsrthhavSe pyrsovteenmto be especially suited to study the chemical comSpcosieitinoncoefsthe atmosphere and to determine the vertical distribution of atmospheric constituents. Approach (Goldman et al, 1973) to the simultaneous analysis of observations selected from a whole limb-scan sequence (global-fit, Carlotti, 1988) Both strategies assume horizontal the homogeneity for lines of sight of Ttthhehe epoobrsCteiorrvnyatooiofsnasptm(h1o-esDprheaesrseusmppatninoend). A two-dimensional (2-D) tomographic approach, named geo-fit (Carlotti et al, 2001), was introduced for the MIPAS (Michelson Interferometer for Passive Atmospheric Sounding) experiment in order to overcome the horizontal homogeneity assumption; it can be used for any limb-scanning satellite experiment where the lines of sight of the spectrometer are oriented (and overlap) along the orbit track. With geo-fit the horizontal inhomogeneities are modelled and retrieved through the simultaneous analysis of observations belonging to all the limb-scans measured along a whole orbit.

The MIPAS experiment and operational retrieval methods
Information Load definitions
The horizontal position error
The temperature position error
Simulated retrievals strategy
Propagation to VMR retrievals adopting externally-provided T profiles
Propagation to VMR retrievals adopting retrieved T profiles
Propagation of T -position error
Components of the temperature-position error
Findings
Position error and averaging kernel
Conclusions
Full Text
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