“…As climate conditions change, glacier mass responds accordingly, triggering modifications in the landscape and biogeochemistry of ecosystems at diverse spatial and temporal scales. However, those interpretations may well be shaped by imaginaries of spatial transformations (Watkins, 2015) implanted by changes observed elsewhere, without accounting for the particular nature of the landscapes analyzed, such as the importance of seasonal snow cover or high elevation wetlands on water availability (Buytaert et al, 2006;Ohlanders, Rodriguez, & McPhee, 2013). As mountain glaciers shrink, we may not only lose valuable archives of past climate and culturally relevant landscape features (Thompson, Mosley-Thompson, Davis, & Brecher, 2011) but we may also witness a transformation in the hydrological and biogeochemical cycles that geographers are uniquely poised to appreciate from a truly integrated perspective, using the many tools of observation and methods of tracing over many different scales.…”