Cryospheric Sciences

Image of The Week – Tumbling Rocks

Emma C. Smith May 20, 2016

A 15,000 m³ rockfall during the 2015 summer heat wave at Tour de Ronde summit, Mont Blanc Massif. (Photo credit: Ludovic Ravanel.)

This photo captures a rockfall at the summit of Tour de Ronde, 3792 m above sea level in the Mont Blanc Massif. On 27 August 2015, around 15000 m3 of rock fell from the steep walls of the mountain. Why do mountains crumble ? Rockfalls such as the one on the photo have been linked to thawing permafrost. The exact mechanism that leads to these events is not fully understood, however, it is thought ...[Read More]

When Cryospheric Research Transforms Lives

Kathi Unglert April 22, 2016

My name is Kathi Unglert, and I’m reporting from the EGU 2016 General Assembly as part of the EGU student reporter programme. Below is my second contribution to the Cryosphere Blog – this time about how cryosphere research can have a real impact on people’s lives. Antoni Lewkowicz – he’s famous, according to a comment I overheard in Tuesday’s PICO session on applied geophysics in cryosphere ...[Read More]

Image of The Week – The Ice Your Eyes Can’t See!

Emma C. Smith April 15, 2016

Figure 1: Soil carbon map of the Northern Hemisphere, averaged over top 3 m. Produced using the SiBCASA model, initialised with with spatially varying permafrost carbon density from the NCSCDv2 data set (Figure 6b from Jafarov and Schaefer, 2016 ) .

Ice sheets and glaciers are very visible and much photographed (e.g. here) elements of the Cryosphere but what about the vast, invisible and buried parts? Around a quarter of the land in the Northern hemisphere remains frozen year round, making up a hugely important part of the cryosphere known as permafrost. Permafrost largely exists at high latitudes (e.g. Siberia and the Canadian Arctic) and t ...[Read More]