Abstract

This article examines a method of inter-calibration for MSU-GS imager of the Russian Geostationary Earth Orbit (GEO) satellite Elektro-L No. 2. Since the launch (December 11, 2015), the satellite's radiation cooler has been operating in an abnormal mode, so the calibration of the IR channels of the MSU-GS imager differed from that pre-flight and, in general, could have a daily variability. To ensure the satellite’s further operation in orbit, it was necessary to calibrate imager channels at a frequency that would allow to identify daily calibration course to detect and compensate its sources. In order to do this, we have developed a special method of GEO-GEO inter-calibration. The calibration of MSU-GS was performed using SEVIRI imager installed on the GEO satellite Meteosat-10. SEVIRI was chosen as a reference instrument because its spectral channels are similar to those of MSU-GS. The MSU-GS was calibrated according to the regressions calculated from the simultaneously images of the field of regard selected between the sub-satellite points. The dynamic brightness temperature (BT) range was determined by deep convective clouds in high troposphere and warm ocean surface. Using the proposed method of inter-calibration, it was possible to confirm the absence of a significant daily variation of the calibration since November 2017. The amplitude of the variation smoothly increases from ~0.2K at high (~ 300K) BTs to ~ 1.0K when the temperature decreased to 200K. These estimates allow the use of the Fourier spectrometer IKFS 2 installed on the Russian Low-Earth-Orbit (LEO) satellite Meteor-M No. 2 to verify the developed GEO-GEO scheme of inter-calibration. Despite the specifics of the situation on board Elektro-L No. 2, the proposed method of GEO-GEO inter-calibration can be applied to radiometers of other neighboring satellites that differ in SSP and spatial resolution.

Highlights

  • Remote sensing data from Geostationary Earth Orbit (GEO) satellites are widely used for continuous monitoring of the atmosphere, ocean and the land

  • There is a need for inter-calibration of satellite instruments directly in the orbit, when measurements from one device are verified by measurements from a reference instrument, which is installed on another satellite, with more accurate and stable radiometric characteristics

  • The calibration differences T = TMSU − TSEV were obtained through the TSEV(TMSU) regression relationships during simultaneous sessions of MSU-GS and SEVIRI on the fixed grid for brightness temperature (BT) more than Tmin

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Summary

Introduction

Remote sensing data from Geostationary Earth Orbit (GEO) satellites are widely used for continuous monitoring of the atmosphere, ocean and the land. Occasionally the radiometric characteristics of the on-board imagers can change due to the degradation of the photosensitive elements or the instability of their operating conditions. Most often within the GSICS, GEO-LEO inter-calibration is carried out (Chander et al, 2013) when a calibrated instrument is onboard a GEO satellite. In this case, the reference instruments is installed on a Low-Earth-Orbit (LEO) satellite. The data of IR channels of the MSU-GS imager were compared with the data of the Atmospheric Infra-Red Sounder (AIRS, Gunshor et al, 2009) that is one of the GSICS reference instruments installed onboard the LEO satellite EOS/Aqua. SEVIRI is installed on the European geostationary satellite Meteosat-10 (with the Sub-Satellite Points (SSP) at the Greenwich meridian over the Atlantic Ocean), and its spectral channels are similar to those of MSU-GS

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