Fig. 2: Long-term surface mass balance components and spatial trends.
From: Poleward shift of subtropical highs drives Patagonian glacier mass loss
Long-term average of (a) total precipitation, (b) surface runoff and (c) surface mass balance (SMB) as modelled by MAR, statistically downscaled to 500 m, for the period 1940-2023. d–f same as a–c but for long-term trends (1940-2023). The background hillshade is derived from the Shuttle Radar Topography Mission (SRTM)30 digital elevation model (DEM) down-sampled to 250 m spatial resolution.
