The Earth’s outgoing radiation is one of the key parameters in the global climate change. This study aims to analyze the feasibility of reconstructing global Earth’s outgoing radiation using disk-integrated measurements. We utilized Clouds and the Earth’s Radiant Energy System (CERES) Synoptic Radiative Fluxes and Clouds (SYN) datasets to simulate the disk-integrated measurements from sensors onboard a Moon-based platform, a satellite at the Sun-Earth Lagrange L1 point, the L2 point, and a polar orbit at the altitude of 380000 km. The reconstruction method is proposed based on the disk-integrated measurements. The results indicated that while the reconstructed radiation at the Sun-Earth L1 point is generally higher than the true value, the radiation reconstructed by the Moon-based and high polar orbit platforms is closer to the true value. Furthermore, we found that the sampling time interval significantly affects the reconstruction accuracy, with intervals of less than 4 hours introducing minimal errors. Our findings suggest that disk-integrated measurements are capable of effectively reconstructing Earth’s global radiation, offering significant guidance for the planning of future missions.
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