Clouds and the Earth’s Radiant Energy System (CERES) Energy Balanced and Filled (EBAF) Top-of-Atmosphere (TOA) Edition-4.0 Data Product

By Norman G. Loeb, David R. Doelling, Hailan Wang, Wenying Su, C. Nguyen, J. G. Corbett, Lusheng Liang, Cristian Mitrescu, Fred G. Rose, Seiji Kato. 2018

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The Max Planck Institute Grand Ensemble: Enabling the Exploration of Climate System Variability (2019, background): “Here the most robust estimate is a single observational estimate of the variability, based on the Clouds and the Earth's Radiant Energy System Energy Balanced and Filled (Loeb et al., 2018) top of the atmosphere irradiance product, which only covers the period 2000–2015.”
The Australian Earth System Model: ACCESS-ESM1.5 (2020, background): “…values are of the correct relative order, with the NH value smaller than the global value and the southern hemisphere (SH) value larger, but with an overall greater gradient (3.69Wm 2) than that seen in present-day observations such as CERES satellite based data (1.30Wm 2) (Loeb et al. 2018).”
Measuring Global Ocean Heat Content to Estimate the Earth Energy Imbalance (2019, background): “Direct measurements of EEI from CERES EBAF are known for their high temporal stability (±0.17 Wm−2 at interannual time scales, Loeb et al., 2018a), reflecting essentially internal climate variability, such as induced by ENSO (Loeb et al., 2017).”