Abstract

The Fengyun-3D (FY-3D) satellite is a Chinese Earth observation satellite with high spectral resolution that can provide multi-spectral observations under all weather conditions. Outgoing longwave radiation (OLR) is an important parameter in the earth radiation energy balance and can reflect changes in atmospheric circulation and convective activity in response to incoming solar radiation. To apply the OLR data of the FY-3D satellite (F_OLR) to weather and climate analyses, the traditional single-channel OLR inversion algorithm for the NOAA (National Oceanic and Atmospheric Administration) satellite was used to calculate F_OLR, and the difference between F_OLR and the OLR data of the NOAA 18 satellite (N_OLR) was analyzed. A correction algorithm was proposed to correct F_OLR to match N_OLR; the spatiotemporal consistency of the corrected F_OLR and N_OLR was evaluated, and the two types of OLR data were used to analyze the onset of the South China Sea Summer Monsoon (SCSSM) and typhoon precipitation in China. The results showed that the corrected F_OLR and N_OLR were consistent in both temporal variation and spatial distribution and that the monitoring of the SCSSM and typhoon precipitation by the two types of OLR data was also in agreement, showing their equivalent quality. Finally, the N_OLR (2006–2019) and the corrected F_OLR (2020-present) were combined to form a long time series OLR dataset that was used in the Beijing Climate Center climate monitoring system in China to monitor abnormal changes in the global convective activity. This study can provide a reference method for future weather and climate applications of Chinese satellites.

Highlights

  • Outgoing longwave radiation (OLR) is defined as the total outgoing radiation flux emitted from the earth’s surface and atmosphere at infrared wavelengths

  • The results showed that the corrected F_OLR and NOAA OLR data (N_OLR) were consistent in both temporal variation and spatial distribution and that the monitoring of the South China Sea Summer Monsoon (SCSSM) and typhoon precipitation by the two types of OLR data was in agreement, showing their equivalent quality

  • F_OLR (2020-present) were combined to form a long time series OLR dataset that was used in the Beijing Climate Center climate monitoring system in China to monitor abnormal changes in the global convective activity

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Summary

Introduction

Outgoing longwave radiation (OLR) is defined as the total outgoing radiation flux emitted from the earth’s surface and atmosphere at infrared wavelengths. OLR is an important parameter of the earth radiation energy balance. OLR has been used to investigate various weather and climate effects, such as large-scale monsoon circulation and monsoon rainfall in most of the tropics and subtropics of East Asia [2,3,4,5], the convective activities in tropical regions [6,7], cloud feedback mechanisms [8,9], and climate model applications [10,11]. For the ERB (Earth’s Radiation Budget) instrument onboard the NOAA and NIMBUS (series of meteorological satellites) and the CERES (Clouds and the Earth’s Radiant Energy System) instrument onboard the Aqua and Terra satellites, OLR was obtained from broadband radiometers. For the AVHRR (Advanced Very High Resolution Radiometer) instrument onboard the NOAA satellite, the VISSR (Visible Infrared Spin Scan Radiometer) instrument onboard the GOES (Geostationary Operational Environmental Satellite) and Fengyu-2 (FY-2) satellites, the SEVIRI

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