Cryospheric Sciences

Icequakes, the little brothers of earthquakes, what do they tell us about ice flow?

Sofia-Katerina Kufner April 24, 2020

Figure 1: Location of Rutford Ice Stream (inset, top), the 2019/2020 field team (inset, bottom) and our camp in the shade of Mount Vinson, Antarctica’s highest peak at 4892 metres. Figure courtesy of Mike Kendall and Sofia Kufner.

Each day, several tens of tiny earthquakes happen beneath Rutford Ice Stream in Antarctica. These events are so small that no human would be able to feel them – yet, scientists can use recordings of these so-called “icequakes” to obtain valuable information on the way ice flows in Antarctica. Read on to find out how… What are icequakes? So we’ve all heard of earthquakes, but what ...[Read More]

For dummies – About ice sheet models and their cold relationship to climate models

Konstanze Haubner April 17, 2020

Climate models help us understand processes occurring in and between atmosphere, oceans, land and ice-covered regions of our planet. One important process impacting all of us is sea level rise, and the ice sheets of Antarctica and Greenland (currently losing more and more ice) play a crucial role in future sea level rise projections. Even though climate models can be very complex and include many ...[Read More]

Did you know… the difference between sea-ice area and sea-ice extent?

Clara Burgard April 10, 2020

Fig. 1: Sea-ice landscape [Credit: Tapio Haaja on Unsplash]

At the beginning of March, just over a month ago, sea ice in the Arctic reached its annual maximum extent. As currently all media attention is focused on other news, you might have missed that, once again, this maximum fell below the 1981 to 2010 average maximum extent. When reading headlines about such sea-ice facts, you may have been confused by the seemingly interchangeable use of “sea-ice exte ...[Read More]

Does debris cover offset glacier retreat in the Greater Caucasus?

Levan Tielidze April 3, 2020

Figure 1: Supra-glacial debris cover (SDC) change on the Elbrus Massif from 1986 to 2014. A SPOT-7 image is used as the background. Blue shows retreat of clean-ice parts. Clean ice in 1986 consists of the clean ice in 2014 (grey, transparent) plus clean-ice area that retreated between 1986 and 2014 (dark blue). Credit: Tielidze et al., 2020

In this week’s blog, Levan Tielidze tells us about supra-glacial debris cover change for the Greater Caucasus. His recent study indicates more than a doubling in the area of supra-glacial debris cover for the Elbrus Massif‘s glaciers from 1986 to 2014, the largest glacierized massif in the whole region. Glaciers on the western slope of the Elbrus Massif are affected by avalanches and thus ar ...[Read More]

Life of a scientist: When fieldwork doesn’t go to plan…

Isobel Rowell March 27, 2020

Climate research questions tend to focus on the future. What will global temperature be in 2100? Will extreme weather events become more frequent? When will sea level rise render coastal homes uninhabitable? But our understanding of climate processes first comes from observing the past: palaeoclimatology. To get these records, scientists often go on fieldwork to collect samples. But what happens w ...[Read More]

Radiocarbon rocks! – How rocks can tell us about the history of an ice sheet…

Keir Nichols March 20, 2020

Figure 1: Collecting a bedrock sample from the Lassiter Coast, Antarctica [Credit: Joanne Johnson, British Antarctic Survey].

When most people hear the phrase “radiocarbon dating”, they think of measuring carbon to date organic material. But did you know that carbon is also produced within rocks, and that we can use it to learn about the past behaviour of a glacier? About 20,000 years ago it was colder and large parts of the continents were covered by ice. But what did Antarctica – the largest ice mass ...[Read More]

What’s up on Thwaites Glacier?

David Docquier March 13, 2020

Figure 1: Map showing the location of Thwaites Glacier in West Antarctica, as well as the main geographic focus of the 8 projects involved in the International Thwaites Glacier Collaboration (ITGC). Credit: ITGC website.

With the West Antarctic Ice Sheet currently losing ice at a fast pace, leading to sea-level rise, it is very important to better understand the processes by which this ice melting occurs. In this context, Thwaites Glacier is a very good case study of an accelerating glacier, which contributes substantially to sea-level rise, and for which a huge scientific collaboration effort has recently been se ...[Read More]

Trapped in the sea ice – Educating the future generations of polar scientists

Thomas Rackow and Friederike Krüger March 6, 2020

In October 2019, the research icebreaker ‘Polarstern’ was moored to an ice floe for its year-long journey through the Arctic Ocean. Come with us on a slightly shorter journey and learn how MOSAiC participants from the supporting cruise educate the future generation of polar scientists! What is the MOSAiC expedition? The MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate ...[Read More]

Boom and bust beneath the ice

Rebecca de Leij February 28, 2020

Beneath the frozen surface of the Southern Ocean, live some of the most spectacular creatures on earth. These creatures are spectacular not only in appearance, but also in their ability to survive in such an extreme environment as Antarctica. Here, temperatures deviate only slightly from 0°C, and food is scarce during the winter months. How do these diverse creatures live in these conditions and w ...[Read More]

The foot of a glaciated mammoth? No… A glacier!

Marie Cavitte February 21, 2020

Elephant Foot Glacier, Greenland. Credit: Ole Zeising (distributed via imaggeo)

Ice is a viscous fluid: it flows but slowly, reaching up to 100 m/yr for the fastest flowing ice. That’s 0.00001 km/hr, so you’d never see it with the naked eye. But what influences the morphology of the glaciers is the shape of the topography that lies underneath them. Elephant Foot Glacier, shown above, aptly named for its shape, is a textbook-example of a piedmont glacier. These types of glacie ...[Read More]