Fig. 3: Two-dimensional histograms showing the probability of a given layer prominence occurring for a given climate condition.
From: Extreme melt season ice layers reduce firn permeability across Greenland
Darker greens indicated higher probabilities. Greenland regions are defined by the dashed boxes in Fig. 2c. a Correlation with the standard deviation of the modeled daily surface-melt production from January 1, 2012 to December 1, 2012 (see “Methods” section). b Correlation with the ratio of latent heat in the total 2012 summer melt to firn cold content in June 2012 in Northwest Greenland. c Same metric for Southern Greenland.
