Abstract

Abstract. Spatially heterogeneous Earth radiance scenes affect the atmospheric composition measurements of high-resolution Earth observation spectrometer missions. The scene heterogeneity creates a pseudo-random deformation of the instrument spectral response function (ISRF). The ISRF is the direct link between the forward radiative transfer model, used to retrieve the atmospheric state, and the spectra measured by the instrument. Hence, distortions of the ISRF owing to radiometric inhomogeneity of the imaged Earth scene will degrade the precision of the Level-2 retrievals. Therefore, the spectral requirements of an instrument are often parameterized in the knowledge of the ISRF over non-uniform scenes in terms of shape, centroid position of the spectral channel and the full width at half maximum (FWHM). The Sentinel-5/UVNS instrument is the first push-broom spectrometer that makes use of a concept referred to as a slit homogenizer (SH) for the mitigation of spatially non-uniform scenes. This is done by employing a spectrometer slit formed by two parallel mirrors scrambling the scene in the along track direction (ALT) and hence averaging the scene contrast only in the spectral direction. The flat mirrors do not affect imaging in the across track direction (ACT) and thus preserve the spatial information in that direction. The multiple reflections inside the SH act as coherent virtual light sources and the resulting interference pattern at the SH exit plane can be described by simulations using scalar diffraction theory. By homogenizing the slit illumination, the SH strongly modifies the spectrograph pupil illumination as a function of the input scene. In this work we investigate the impact and strength of the variations of the spectrograph pupil illumination for different scene cases and quantify the impact on the ISRF stability for different types of aberration present in the spectrograph optics.

Highlights

  • The Ozone Monitoring Instrument (OMI) was the first instrument identifying the issue arising from non-uniform Earth scenes on the shape and maximum position of the spectral response of the instrument (Voors et al, 2006)

  • We present the instrument spectral response function (ISRF) figures of merit resulting from the simulation of several Zernike polynomials for the Sentinel-5/UVNS applicable heterogeneous Earth scene and a 50 % stationary calibration scene

  • All Zernike polynomials increase the error in the ISRF knowledge compared to the case where the ISRF is calculated as the convolution with a constant gaussian point spread function (PSF)

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Summary

Introduction

The Ozone Monitoring Instrument (OMI) was the first instrument identifying the issue arising from non-uniform Earth scenes on the shape and maximum position of the spectral response of the instrument (Voors et al, 2006). Whenever the in-orbit ISRF shape deviates from the on-ground characterized shape due to, for example, heterogeneous scenes, it will affect the measured spectrum from which the Level-2 products are retrieved (e.g., CH4 and CO in the SWIR-3 channel of Sentinel-5/UVNS). This effect is prominent for instruments with a high spatial resolution. Recent high-resolution hyperspectral imaging spectrometers with an IFOV comparable to the sampling distance (or scan area) are more strongly affected and demand a set of stringent requirements on the in-flight knowledge and stability of the ISRF This is necessary, as distortions in the ISRF due to non-uniform scenes will introduce biases and pseudo-random noise in the Level-2 data and in the precision of atmospheric composition products.

Slit homogenizer model
Near field
Far field
Collimator astigmatism
Diffraction grating
Spectrograph pupil intensity distribution
Impact on ISRF
Results and discussion
Conclusion
Full Text
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