EGU Guest blogger

Water plumes are tickling the Greenland Ice Sheet

Johanna Beckmann January 31, 2020

Figure 1. Cross section of a schematic representation of a glacier. Surface water is penetrating into the glacier through crevasses at its surface, reaching its base where it flows towards the ocean. Once this freshwater has entered the ocean, it rises up creating a so-called water plume. Credit: Stefan Hollenbach.

7 meters of sea-level rise – what you would get if the whole Greenland Ice Sheet melted. But the tricky question is: how much of this ice will be melted in the next decades, and how fast will it occur? This piece of information is critical in order to plan for present and future populations living in coastline areas, all around the world. How much and how fast can the Greenland Ice Sheet melt ? In ...[Read More]

Climate Change & Cryosphere – The fate of Georgian Glaciers

Levan Tielidze January 24, 2020

Display "The fate of Georgian Glaciers" from YouTube Click here to display content from YouTube. Learn more in YouTube’s privacy policy. Always display content from YouTube Open "The fate of Georgian Glaciers" directly Last week, we learned about the dramatic fate of the Hochjochferner, which has strongly retreated in the past years due to climate change. It represented just on ...[Read More]

Education in glaciology: Witnessing the death of a glacier

Olaf Eisen and Carleen Tijm-Reijmer January 17, 2020

Fig.1. View of the Hochjochferner and its prominent medial moraine during the “Almabtrieb” in September 2003. The bumps on the glacier are from support pillars of a ski lift. Photo credit: Carleen Tijm-Reijmer

The Karthaus summer school on Glaciers and Ice Sheets in the Climate System has a long history of training many generations of PhD students, thus forming professional networks that have lasted throughout their careers. The Karthaus summer school has been described in detail in a previous Cryoblog post. Here we want to focus on the story of a glacier… Hochjochferner, a retreating glacier One ...[Read More]

Did you know? – Ocean bathymetry can control Antarctic mass loss!

Sainan Sun January 10, 2020

Ice shelves (the floating parts of the Antarctic ice sheet) play a fundamental role in the stability of the Antarctic ice sheet (see this post) and, therefore, its contribution to global sea-level rise. They lose mass primarily through melting at their bases, which are in contact with the ocean. This thins them and makes them more vulnerable, reducing their stabilising potential and causing more i ...[Read More]

Cryo History – How airborne glaciologists measured the movement of glaciers before the satellite era

Niels Korsgaard and Baptiste Vandecrux December 13, 2019

Recent work published in my department at the Geological Survey of Denmark and Greenland (GEUS) focused on solid ice discharge into the ocean from the Greenland Ice Sheet from 1986 to 2017 (Mankoff et al. 2019). Solid ice discharge is the ice that is lost from a glacier as it flows towards the coast and eventually breaks off as icebergs into the ocean (i.e. calving). Solid ice discharge is an impo ...[Read More]

Cryo Adventures – What’s currently going on in Antarctic science?

Andy Smedley, Jenny Arthur and Sofia Kufner December 6, 2019

Map of the various locations mentioned in the text. Green markers are bases, red markers measurement campaign locations [Credit: Andy Smedley].

As Christmas gets closer, days are getting shorter in the northern hemisphere. A good excuse to get cosy inside on the sofa, drinking tea and eating Christmas biscuits. Meanwhile, a few thousand of scientists are heading “South”, to Antarctica, where the lengthening days provide the perfect conditions to conduct a whole variety of scientific field expeditions… Science in Antarctica Just last ...[Read More]

Did you know…? Antarctica Day 2019 – 60 years of peace

Jenny Turton November 29, 2019

Figure 1: Scientists fly the flags for the school children who designed them for Antarctica Day [Photo credit: UK Polar Network].

December 1st 2019 marks the 60th anniversary of the signing of the Antarctic treaty. To celebrate the signing of the treaty, ‘Antarctica Day’ now occurs each year on December 1st. But what is the Antarctic Treaty? How do people celebrate? This week’s blog post will tell you everything you need to know, just in time for celebrations! Antarctic Treaty The Antarctic Treaty was originally signed by 12 ...[Read More]

Cryo-Comm – Six reasons why you should communicate your science

Ella Gilbert November 15, 2019

What inspired you to get into polar or cryospheric research? Perhaps it was a passion for the outdoors, a drive to protect the environment for the people and animals that live there, or a fascination with wild places. For me, it was all three – and the more I learned about Antarctic climate science, the more I realised that the polar regions are vital to the functioning of a healthy planet, and so ...[Read More]

Did you know… about the fluctuating past of north-east Greenland?

Ilaria Tabone November 8, 2019

Fig. 1: Map of the north-east sector of Greenland showing the location of the North East Greenland Ice Stream (NEGIS) with its three outlet glaciers (Nioghalvfjerdsfjorden (79N), Zachariae Isstrøm (ZI) and Storstrømmen Glacier (SG)), and the offshore bathymetry and the position of its margin reconstructed for the Last Glacial Maximum (LGM) (dotted black line) [Credit: Ilaria Tabone].

Recent geological data shows that during a very cold phase of our Earth’s climate (between 40,000 and 26,000 years ago), there was a huge expansion of polar ice sheets, yet the north-eastern part of the Greenland ice sheet was less extensive than today. How could this have occurred? In this post we shed light on the potential causes of this ice sheet behaviour. What do we know about present- ...[Read More]

For Dummies – How do wildfires impact permafrost? [OR.. a story of ice and fire]

Jean Holloway November 1, 2019

Wildfire – like the ones observed in the Northwest Territories, Canada in 2014 (Fig. 1) – is a natural part of permafrost landscapes, but fires are expected to get more frequent and severe as the climate warms. This could accelerate the degradation of permafrost, with negative consequences on the local and global scale! We have a pretty good understanding of how permafrost responds to fire t ...[Read More]