Glaciers are some of the best indicators of climate change. Their existence depends on a fine balance between mass accumulation (usually through snowfall) and mass loss (mainly by ablation or melting). Any small increases in mean annual temperature elicit an amplified response in glaciers and can drastically reduce their mass balance – more ice lost than gained. This is why glaciers are responding so rapidly to rising temperatures. However, it isn’t as simple as that; there are a number of complicating factors that alter how fast or slow glaciers respond, some occurring on a case-by-case basis. For scientists to use glaciers as a robust and reliable...