Cryospheric Sciences

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]

An interview with Jean Holloway on the importance of mental health in graduate school

Jean Holloway February 14, 2020

Recent studies have shown that mental health conditions are far more common in graduate students than in the general public (e.g. Bolotnyy et al., 2020). Despite the prevalence, these issues are not something that are often openly discussed, and graduate students often don’t seek treatment. This week, we are interviewing Jean Holloway who aims to shed some light on her personal experience with som ...[Read More]

Climate Change & Cryosphere – The tropical fingerprint in Arctic climate

Michelle McCrystall February 7, 2020

Figure 1: A schematic to illustrate an atmospheric bridge whereby connecting one part of the climate system with another [Credit: M. McCrystall].

We know that climate change is being felt worldwide, but it is especially prominent in the Arctic, where temperatures are warming twice as fast as anywhere else on the planet. This especially sensitive environment, whose icy, snow-covered land and sea is so important in the global climate system, is really starting to feel the heat. But where is this heat coming from? In this blog post, we will ex ...[Read More]

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]