Abstract

Abstract. SCIAMACHY (SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY) on-board the European Environmental Satellite (Envisat) provided spectrally resolved measurements in the wavelength range from 0.24 to 2.4 µm by looking into the Earth's atmosphere using different viewing geometries (limb, nadir, solar, and lunar occultation). These observations were used to derive a multitude of parameters, in particular atmospheric trace gas amounts. In addition to radiance measurements solar spectral irradiances (SSIs) were measured on a daily basis. The instrument was operating for nearly a decade, from August 2002 to April 2012. Due to the harsh space environment, it suffered from continuous optical degradation. As part of recent radiometric calibration activities an optical (physical) model was introduced that describes the behaviour of the scanner unit of SCIAMACHY with time (Krijger et al., 2014). This model approach accounts for optical degradation by assuming contamination layers on optical surfaces in the scanner unit. The variation in layer thicknesses of the various optical components is determined from the combination of solar measurements from different monitoring light paths available for SCIAMACHY. In this paper, we present an optimisation of this degradation correction approach, which in particular improves the solar spectral data. An essential part of the modification is the use of measurements from SCIAMACHY's internal white light source (WLS) in combination with direct solar measurements. The WLS, as an independent light source, therefore, gives an opportunity to better separate instrument variations and natural solar variability. However, the WLS emission depends on its burning time and changes with time as well. To use these measurements in the optimised degradation correction, the change in the WLS emission in space needs to be characterised first. The changes in the WLS with accumulated burning time are in good agreement with detailed laboratory lamp studies by Sperling et al. (1996). Although the optimised degradation-corrected SCIAMACHY SSIs still show some instrumental issues when compared to SSI measurements from other instruments and model reconstructions, our study demonstrates the potential for the use of an internal WLS for degradation monitoring.

Highlights

  • In order to understand the Earth’s climate and its changes, the Earth’s atmosphere has been studied by numerous instruments from space since the 1970s

  • Some new artefacts are visible, e.g. at the beginning of 2011. They seem to originate in the azimuth scan mechanisms (ASM) diffuser solar spectra and are transferred to the ESM diffuser solar spectra and white light source (WLS) spectra through their simultaneous fit in the degradation modelling

  • Beginning with the lowest wavelength band centred at 330 nm, the SCIAMACHY solar spectral irradiances (SSIs) time series lies within the solar cycle variation in SATIRE-S and SIM V25 data sets

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Summary

Introduction

In order to understand the Earth’s climate and its changes, the Earth’s atmosphere has been studied by numerous instruments from space since the 1970s. Recent studies (Mauceri et al, 2018; Woods et al, 2018, 2015) indicate that the UV variations in SIM/SORCE were initially overestimated and these solar irradiance changes are consistent with possible instrument sensitivity drifts (Lean and DeLand, 2012). One challenge for space-based measurements is the harsh environment of operation (vacuum, high energetic particles, temperature extremes, ultraviolet radiation, etc.) Among other things, this environment can cause relatively rapid degradation of the satellite instruments, which becomes problematic in particular when measuring over long periods The degradation is derived relative to a reference measurement with published absolute calibration (Hilbig et al, 2018) This is achieved by adaption of the degradation correction for the SCIAMACHY instrument by modifying the mirror model approach (Krijger et al, 2014) as described in Sect.

SCIAMACHY measurements from 2002 to 2012
Instrument
Solar measurements
Calibration
Starting point: in-flight degradation correction approaches for SCIAMACHY
Modifications for solar applications
ASM diffuser solar measurements
WLS ageing correction
Iterative degradation fit
The recalibrated SCIAMACHY SSI
Comparison with SCIAMACHY SSI
SSI reconstructions
SSI time series
Findings
Summary and conclusions
Full Text
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