Justin PF Pomeranz

Abstract INTRODUCTION RESULTS AND DISCUSSION MATERIALS AND METHODS Acknowledgments Supplementary Materials REFERENCES Information & Authors Metrics & Citations View Options References Figures Tables Media Share Abstract Cryospheric landforms play a critical role in alpine hydrology and ecosystems.

Figure S1. The edges of the first 4 bins are shown when the body sizes range from 0 to 100 (bottom line) and 0–1000 (top line). Figure S2. The edges of all bins for the L2n method are shown when body sizes range from 0 to 100 (bottom line) and 0–1000 (top line). Figure S3. The variation in the distributions of λ $$ \lambda $$ estimates for “steep” values in Figure 2 in the main text makes it difficult to compare them with the “shallower” distirbutions. Figure S4.