Third pole darkening affects local and remote climates, finds study NatureComms
. For CTL_t and CTL_e, the climate forcing was derived from the downscaled near-surface air temperature and precipitation of CTL. The climate data from SCE was also downscaled using the same correction procedure as was applied to the climate data of CTL to drive SCE_t and SCE_e simulations. Thereby, the difference in the climate between CTL and SCE is well preserved in the climate forcing of CTL_t and SCE_t simulations.
To estimate the albedo-induced glacier changes on the centennial scale, we computed the difference in glacier properties between last year’s results of SCE_t and CTL_t. Similarly, the difference in glacier properties between the final 1000-year-average results of SCE_e and CTL_e was used to represent the albedo-induced changes in glaciers at the equilibrium state. Since some glaciers were not well captured by OGGM, we then upscaled the glacier volume and area through the scaling factor.
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