Fig. 5: Emergence of externally forced change from natural climate variability in reanalysis datasets over different continents.
From: Can climate change signals be detected from the terrestrial water storage at daily timescale?
The fraction of days in which climate change signals have emerged from natural variability (that is, below the 2.5th percentile in the multi-model 1861–1950 distribution) in Africa (a), Asia (b), Australia (c), Europe (d), North America (e), and South America (f).
