Greenland
WHERE? The glaciated catchment of Ilulissat, terminating in an ice-marginal lake system, is ca. 187 km2. In contrast, ice sheet catchment above Kangerlussuaq is distinct as the sole large-scale ice sheet catchment with open access river discharge data. The glaciated part of the catchment is ca. 2260 km2, and the ice-free part is 630 km2.
WHY? LIQUIDICE explores the critical role of Greenland’s ice sheet meltwater in global sea level rise, local marine ecosystems, and sustainable energy production. With meltwater runoff increasing by up to 80% in Southwest Greenland over the past 40 years, our research focuses on two key glaciated catchments—one vital for local hydropower in Ilulissat and the other essential for refining climate
models. By advancing our understanding of future meltwater dynamics, LIQUIDICE supports Greenland’s green transition and contributes to global climate predictions.