absorption is often the dominant melt energy source for snow and ice on land,
glaciers, sea, and lakes. Snow and ice melt feedbacks play a role in Arctic
amplification of climate warming.
This project is to evaluate the 2017 and 2018
seasonal variations in Greenland snow optical properties using imagery from the
Copernicus ESA Sentinel-3 A and B satellite platforms.
The work involves the
use of a scientific programming language, e.g. Matlab or IDL and may benefit
The project may include travel support to attend ESA meetings.
DTU supervisor could be an employee from DTU Space.
In collaboration withGEUS / Jason E. Box (email@example.com)
Scientific data analysis using Matlab, IDL or equivalent