Cryosphere



The cryospheric topic aims to improve the understanding of the processes and dynamics of different components of the cryosphere, namely land ice, ice shelves, glaciers, snow, sea ice and permafrost. To this end, the cryosphere team focusses on the following research goals:

  • What are the contributions of glaciers, ice caps and polar ice sheets to the rise in sea level and what is the nature of the influence of climate change on their mass balance and dynamics?
  • What do the distributions of the extent, thickness and other physical characteristics of sea ice look like and how do they react to climate variability and change?
  • How do changes in the snow and ice masses influence the surface energy balance and the circulation of the atmosphere and the ocean?
  • Which spatial and temporal changes in the snow and ice extent and mass are to be expected on the continents in the coming decades, and how will these influence the water budget, ecology and biodiversity?
  • How does climatic change affect the stability of permafrost and the annual freeze and thaw dynamics?
  • What are the ecosystem responses to degrading permafrost and what are the impacts on the Arctic carbon cycle?
  • How does the components of the cryosphere interact and are there relevant feedback mechanisms between sea ice, snow cover and permafrost?
  • Can changes in the cryosphere trigger abrupt or critical changes in the world’s climate system?

The combination of remote sensing, field surveys and modelling is the approach to answer these questions. Besides monitoring, the evaluation of essential variables from SAR systems allows to greatly improve understanding of processes and systems and is thus of crucial importance. SAR systems operating at X- and L-Band, used in synergy with each other, can greatly improve the knowledge of dynamics and stability of components of the cryosphere.


 


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