https://iopscience.iop.org/article/10.1088/1748-9326/ae8a67
Authors: Gianni Bellocchi, Vinay Kumar, Fredrik Charpentier Ljungqvist and Nazzareno Diodato
22 July 2026
DOI 10.1088/1748-9326/ae8a67
Abstract
Earth has reflected progressively less solar radiation since the start of the satellite era (1979), amplifying the planetary energy imbalance. Satellite analyses attribute the trend primarily to circulation-driven contraction of reflective cloud regimes, whereas process-based studies emphasize surface reflectivity changes. We argue that these perspectives are dynamically linked: as cloud cover contracts, diminishing atmospheric masking elevates the realized climatic leverage of surface albedo. This coupling makes surface reflectivity an increasingly important and manageable regulator of solar absorption under clearer-sky conditions. We propose an integrated governance framework that explicitly incorporates albedo management alongside carbon management.
Source: IOP Science