Cryospheric Sciences

European Space Agency Living Planet Symposium 2016

Stephen Chuter May 26, 2016

Background: Prague Castle as viewed from the Charles Bridge (Credit: Stephen Chuter)

Living Planet Symposium Between the 9th and 13th May, Prague played host to the European Space Agency’s (ESA) fourth Living Planet Symposium. The event, the largest in its history with over 3300 attendees, brought together the earth observation community across multiple disciplines to discuss significant scientific results and the future developments of earth observation missions. Earth Observatio ...[Read More]

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]

Image of the Week – See How Seasonal Sea Ice Decline Differs!

Clara Burgard May 13, 2016

Figure 1: Arctic sea-ice area (75°N to 90°N) VS global annual mean surface air temperature for the complex model MPI-ESM-LR. Red dots represent a seasonal average over autumn (September/October/November) and blue dots over spring (March/April/May) of a particular year in the historical and future (RCP8.5) simulations. The dotted black lines result from a linear orthogonal regression in the ice area regime with the steepest change (Credit: subset of fig 2 from Bathiany et al, 2016 ).

Why do we care about sea ice in the first place? Sea ice is important for several components of the climate system. Due to its high albedo, sea ice reflects a high amount of the incoming solar radiation and is therefore relevant for the Earth’s energy budget. Sea ice inhibits the exchange of heat, moisture and momentum between ocean and atmosphere, which usually occur at the sea surface. Whe ...[Read More]

From Hot to Cold – Volcanology Meets the Cryosphere

Kathi Unglert May 10, 2016

Hello again, I’m Kathi Unglert, and you’re about to read my third and final post as a student reporter at EGU 2016. Today I am writing about my experience in the cryosphere sessions from my volcanology perspective. In preparation for the conference I kept thinking about what sort of research I would see in the cryosphere sessions. I had never really attended any specific conferences or meetings on ...[Read More]

Image of the Week — Glowing Ice

Sophie Berger May 6, 2016

Glowing ice -- winning picture of the EGU photo contest 2016. The image shows a block of ice on the shores of Jökulsárlón, Iceland. [credit: Katharine Cashman (distributed via imaggeo.egu.eu)]

Two weeks ago, the EGU General Assembly was coming to an end in Vienna. With over 16,500 participants, this year’s edition was bigger and more varied than ever (e.g check out this good overview of the science-policy short course, published 2 days ago on geolog). The week was particularly fruitful for the cryospheric sciences and to mark this we have cherry-picked one of the winning picture o ...[Read More]

Careers at the European Space Agency – How and Why?

Anna Maria Trofaier & Anna Hogg May 3, 2016

Flow speed of Jakobshavn Isbræ outlet glacier (South West Greenland) in winter 2014. Credit: ESA

As the pace of modern life speeds up and job competition becomes even more fierce, it is good to have a focused plan of where you would like to be in the future. The European Space Agency (ESA) offers traineeships and research positions to young scientists on a regular basis. They may be a springboard into your chosen career path, but how do you go about bagging one of these valuable opportunities ...[Read More]

Image of the Week – Storing water in Antarctica to delay sea-level rise

David Docquier April 29, 2016

Difference in ice thickness from the initial equilibrium state after 100 years of ice addition (upper panels) and 1000 years after the end of the forcing (lower panels). Two scenarios are shown, 200 km (left panels) and 800 km (right panels) from the coastline, both corresponding to a sea-level mitigation of 10 mm per year (credit: Frieler et al., 2016, fig 3) .

Sea level rise Sea-level rise is one of the main impacts of the current global warming and its rate has dramatically increased in the last decades (the current rate is about 3 mm per year). Even if greenhouse gas emissions were stopped today, sea level would continue to rise due to the slow Earth climate system response (IPCC, 2013, chap. 13). It is therefore a considerable threat for popul ...[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 – EGU General Assembly 2016

Emma C. Smith April 22, 2016

The sun sets over the Austria Center Vienna (ACV), where the 2016 EGU General Assembly is being held this week. Photo Credit: Nanna B. Karlsson.

The EGU General Assembly, which takes place each year in Vienna, Austria, draws to a close today. Attended by nearly 13,650 participants from 111 countries, with around a third of those being students – a great turn-out for this vital part of the early career scientists (ECS) community! It has been a very productive meeting for the cryosphere division with a huge number and variety of oral ...[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]