Fig. 2: Albedo-induced boreal summer precipitation changes.
From: Regional and tele-connected impacts of the Tibetan Plateau surface darkening
a The spatial pattern of albedo-induced boreal summer precipitation changes in eastern Eurasia. The stippling indicates a significant difference (p < 0.05, non-parametric Wilcoxon signed-rank test). The boundaries of six subdivision regions, including South Asia (SA), the Indian subcontinent core monsoon region (ICR), Northeast Asia (NEA), North China (NC), the Yangtze River Valley (YTR), and South China (SC), are highlighted by black dashed lines. The regional averaged boreal summer precipitation in these six subdivision regions is shown in panel (b). The unit of the scale in the radar plot is mm day−1. More details about these regions are shown in the Methods.
