Source Themes

DEEP-C Consortium: Carbon sink or methane source–local to global scale assessment of lentic waters’ role in the climate system
Half of the soil erosion in the Alps during the Holocene is explained by transient erosion crises as a consequence of rapid human land clearing
Quantifying the impacts of landscape opening on alpine soil erosion dynamics during the Holocene
Past and future climate change effects on thermal regime and oxygen solubility of four peri-alpine lakes
Quantifying soil erosion during the Holocene by coupling land surface modeling and paleoenvironmental approaches
Quantifying soil erosion during the Holocene by coupling land surface modeling and paleoenvironmental approaches