Abstract

A common way to regularize mathematical ill-posed retrieval problems in atmospheric remote sensing is the incorporation of single-spectrum Bayesian a priori mean values and standard deviations for the parameters to be retrieved, along with measurement and simulation error information. This decreases the probability to obtain unlikely parameter values. For a reliable evaluation of measurements with sparse spectral information content like Venus' nightside emissions in the infrared as acquired by the VIRTIS-M-IR instrument aboard ESA's Venus Express spacecraft, it can help to consider further a priori knowledge.A new multi-spectrum retrieval technique (MSR) is presented that allows one to incorporate expected correlation lengths and times for the retrieval parameters used to describe several spectra. It is demonstrated by examples that this decreases the probability to retrieve spatial–temporal state vector distributions that are incompatible with these a priori spatial–temporal correlations. Also, a priori correlations between the parameters used to describe a single spectrum and exhibiting similar a priori spatial–temporal behavior, act to rule out unlikely single-spectrum state vectors. Parameters with infinite correlation length or time and identic single-spectrum a priori data are spatially or temporally constant and can be retrieved as parameters that are common to a certain selection of measurements. This is shown to be especially useful to retrieve surface emissivity in the infrared as a parameter that is common to several measurements that repeatedly cover the same target, and to determine deep atmospheric CO2 opacity corrections, which are common to all Venus nightside spectra. Also this way, all considered measurements can be parameterized by a fully consistent set of atmospheric, surface, and instrumental parameters that respects all available a priori data as well as the measurement and simulation error distributions and that does not neglect the context between adjacent measurements. MSR is demonstrated to enhance the retrieval reliability and accuracy and pushes the VIRTIS-M-IR data evaluation to its limits.

Highlights

  • The geology and composition of Venus’ surface are topics of active research

  • It is demonstrated by examples that this decreases the probability to retrieve spatial-temporal state vector distributions that are incompatible with these a priori spatial-temporal correlations

  • This is shown to be especially useful to retrieve surface emissivity in the infrared as parameter that is common to several measurements that repeatedly cover the same target, and to determine deep atmospheric CO2 opacity corrections, which are common to all Venus nightside spectra

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Summary

Introduction

The geology and composition of Venus’ surface are topics of active research. There are only a few in situ measurements, performed by the VENERA probes [1]. For measurements with sparse spectral information content, like the VIRTIS-M-IR measurements of Venus’ nightside emissions, this may seriously degrade the reliability of retrieved single-spectrum parameters To overcome this problem, a multi-spectrum retrieval algorithm (MSR) is presented (Section 2) that allows for the utilization of additional a priori knowledge such as a priori spatial-temporal correlations. A multi-spectrum retrieval algorithm (MSR) is presented (Section 2) that allows for the utilization of additional a priori knowledge such as a priori spatial-temporal correlations These are usually neglected but always present, since contiguous measurements are unlikely to originate from completely unrelated state vectors. The probability distribution function with the least information content (meaning without implying further knowledge) that is consistent with the parameterization by a mean value vector and a covariance matrix, is the corresponding Gaussian [18].

A priori covariance matrix
A priori correlation matrix
Single-parameter problem for several spectra
Positive definite functions
Spherical planetary surface
Spatial-temporal and other separations
Single-spectrum problem for several parameters
Retrieval of common parameters
Forward model
Local parameters
Common parameters
Examples and discussion
Conclusions and outlook
Cost function as least squares norm
Inverse square root of a priori covariance matrix
Limit for perfect spatial-temporal coupling
Further notes on implementation
Full Text
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