A comprehensive inventory of Swiss glacial lakes shows how the lake landscape in the high mountains has changed since the end of the Little Ice Age.
Due to climate change, the glaciers of the Alps are melting. When the sometimes huge ice fields retreat, they often leave behind depressions and natural dams in the exposed landscape. The basins can fill with meltwater and new glacial lakes are formed. Since the end of the Little Ice Age around 1850, almost 1,200 new lakes have been added in formerly glaciated regions in the Swiss Alps. Around 1,000 still exist today. This is shown by a new, comprehensive inventory of all Swiss glacial lakes.
“On the one hand, we were surprised by the sheer numbers and on the other by the marked acceleration in formation,” says Daniel Odermatt, Head of the Remote Sensing Group at the aquatic research institute Eawag. “At the beginning of the project, we expected a few hundred glacial lakes. Now there are over a thousand, and 180 have been added in the last decade alone.” In the team with his postdoc Nico Mölg, together with researchers from the University of Zurich and the Federal Office for the Environment, they have surveyed all the glacial lakes that have formed in the Swiss Alps over the past 170 years or so and recorded various indicators.
Dates go back to the end of the Little Ice Age
The comprehensive inventory was only possible thanks to the high-quality aerial photo data from Swisstopo and many years of data on glaciers in Switzerland. The oldest information dates back to the middle of the 19th century. “When the ice began to melt at the end of the Little Ice Age, it caught the interest of the naturalists at the time,” Mölg explains. “Between 1840 and 1870, the change in extent and length of some large glaciers in the Swiss Alps were therefore mapped for the first time for the Dufour map.” With the “American Aerial Survey” of 1946, the first high-quality aerial photographs became available. In total, the research team was able to draw on data at seven points in time between 1850 and 2016.
For each of the 1,200 lakes, the researchers recorded the location, elevation, shape and area of the lake at the different times. They determined the type and material of the dam, surface drainage and recorded the development of the lake. With this basic information, the next step is to estimate the individual hazard potential of the lakes, such as the risk of the sudden emptying of the lake in the event of a dam failure.