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Can we use TRMM-PR bright band heights to estimate the snow-rain transition in high mountain regions?
(American Geophysical Union, 2015)
Field and modelling based research indicates that for tropical glaciers, variations in snow cover and the altitude of the snow line via albedo effects are among the most crucial factors to explain the differences in annual ...
Acceso abierto
Relevance of future snowfall level height in the Peruvian Andes for glacier loss in the 21st century under different emission scenarios
(American Geophysical Union, 2017)
In many regions of Peru, the competition for limited hydrological resources already represents a large risk for conflicts. In this context, and within the circumstances of climate change, there is a great interest in ...
Acceso abierto