Cryospheric Sciences

Image of The Week – Ice Flows!

Sammie Buzzard March 17, 2017

By changing factors such as snowfall and temperature players can alter the ice flow and make sure that icebergs starts to form just where the penguins want to dive down and catch fish, but get it wrong and there’s a seal waiting! [Credit: Still image from the Ice Flows game]

Portraying ice sheets and shelves to the general public can be tricky. They are in remote locations, meaning the majority of people will never have seen them. They also change over timescales that are often hard to represent without showing dramatic images of more unusual events such as the collapse of the Larsen B Ice Shelf. However, an app launched in the summer at the SCAR (Scientific Committe ...[Read More]

Image of the Week — Hidden lakes in East Antarctica !

Sophie Berger March 10, 2017

Underwater picture of englacial lake 4m below the surface [Credit: S. Lhermitte].

Who would have guessed that such a beautiful picture could get you interviewed for the national news?! Certainly not me! And yet, the photo of this englacial lake (a lake trapped within the ice in Antarctica), or rather science behind it, managed to capture the media attention and brought me, one of the happy co-author of this study, on the Belgian television… But what do we see on the pic ...[Read More]

Quantarctica: Mapping Antarctica has never been so easy!

George Roth March 8, 2017

One of the most time-consuming and stressful parts of any Antarctic research project is simply making a map. Whether it’s plotting your own data points, lines, or images; making the perfect “Figure 1” for your next paper, or replying to a collaborator who says “Just show me a map!,” it seems that quick and effective map-making is a skill that we take for granted. However, finding good map data and ...[Read More]

Image of The Week – The Pulsating Ice Sheet!

Emma C. Smith March 3, 2017

Figure 1: (a) Ice sheet at its most advanced state, the terminus is grounded 300 m beneath sea level (b) An ocean-warming event triggers retreat (c) Retreat is amplified by enhanced calving as the ice sheet retreats into deeper water (d) After the collapse, the ice sheet is in its most retreated position. Isostatic adjustment uplifts the bed (and sill) which will allow the ice sheet to advance again. Insets show a close-up around the sill. [Credit: Bassis et al., 2017]

During the last glacial period (~110,000-12,500 years ago) the Laurentide Ice Sheet (North America) experienced rapid, episodic, mass loss events – known as Heinrich events. These events are particularly curious as they occurred during the colder portions of the last glacial period, when we would intuitively expect large-scale mass loss during warmer times. In order to understand mass loss m ...[Read More]

Image of the Week — The ice blue eye of the Arctic

Céline Heuzé February 24, 2017

Ice floe with a melt pond (light blue patch), observed in Nares Strait , in August 2015 from I/B Oden [Credit: C. Heuzé]

“Positive feedback” is a term that regularly pops up when talking about climate change. It does not mean good news, but rather that climate change causes a phenomenon which it turns exacerbates climate change. The image of this week shows a beautiful melt pond in the Arctic sea ice, which is an example of such positive feedback. What is a melt pond? The Arctic sea ice is typically non-smooth, and ...[Read More]

Image of the Week – Icelandic glaciers monitored from space!

Luca Foresta February 17, 2017

Figure 1: Exceptionally cloud free view of Iceland taken from ESA Envisat on 21, July 2010. Rates of surface elevation change between 2010-2015 derived from ESA CryoSat-2 swath-processed elevations are overlaid over the six largest ice caps. The time series shows thinning below 1200 m elevation over Vatnajökull, the largest ice cap in Iceland and Europe (by volume) -see Foresta et al. (2016) [Credit: L. Foresta and Dr. N. Gourmelen, University of Edinburgh, School of GeoSciences]

Located in the North Atlantic Ocean, just south of the polar circle, Iceland is a highly fascinating land. Covered by some of the largest glaciers in Europe and hosting active volcanoes, geothermal sites and subglacial lakes, it is extremely dynamic in nature and ever changing. With this Image of the Week we will tell you a bit about the changing ice caps of Iceland and how we can monitor them fro ...[Read More]

Image of the Week – Apocalypse snow? … No, it’s sea ice!

Jean-Louis Tison February 10, 2017

Sea-ice brine sampling is sometimes challenging [Credit: Stefan Hendricks]

Sea ice brine sampling is always great fun, but sometimes somewhat challenging ! As sea water freezes to form sea ice, salts in the water are rejected from the ice and concentrate in pockets of very salty water, which are entrapped within the sea ice. These pockets are known as “brines”. Scientists sample these brines to measure the physical and bio-geochemical properties, such as: tem ...[Read More]

Image of the Week – Supraglacial debris variations in space and time!

Morgan Gibson February 3, 2017

Figure 1: A schematic diagram of debris distribution on a debris-covered glacier, showing spatial variation in debris distribution with regards to rock type and layer thickness. Modelled on Baltoro Glacier, Karakoram. Surface velocity, sediment flux and debris thicknesses would vary between glaciers. Click here for a larger version. [Credit: Gibson et al., unpublished]

There is still a huge amount we don’t know about how glaciers respond to climate change. One of the most challenging areas is determining the response of debris-covered glaciers. Previously, we have reported on a number of fieldwork expeditions to debris-covered glaciers but with this Image of The Week we want to show you another way to investigate these complex glaciers – numerical modelling! Deb ...[Read More]

Image of the Week – On the tip of Petermann’s (ice) tongue

Céline Heuzé January 27, 2017

Petermann's ice tongue. [Credit: C. Heuzé]

5th August 2015, 10:30 in the morning. The meeting had to be interrupted to take this picture. We were aboard the Swedish icebreaker Oden, and were now closer than anyone before to the terminus of Petermann Glacier in northwestern Greenland. But we had not travelled that far just for pictures… Petermann’s ice tongue Petermann is one of Greenland’s largest “marine terminating glaciers”. As the name ...[Read More]

Katabatic winds – A load of hot (or cold) air?

Thomas Shaw January 25, 2017

Figure 1: A schematic of the potential wind flow and interplay of local effects on Tsanteleina Glacier in the Italian Alps. The diagram represents wind modelling, measured data and observations from the field. (1) The interactions of down-glacier katabatic winds (blue) and up-valley winds/local heat sources (red); (2) the potential heat emitted from the warm valley surroundings (pink) and; (3) localised surface depressions representing glacier 'cold spots' during calm, high pressure conditions. Arrows correspond to synoptic westerlies (purple), southerly airflow (orange), katabatic winds (blue) and valley winds (red) [Credit: T Shaw, unpublished] - Click here for a larger version.

It might seem obvious that a warming world will lead to a reduction in glacial ice cover, but predicting the response of glaciers to climatic change is no simple task (even within the short term). One way to approach this problem is to come up with relationships which describe how glaciers interact with the world around them, for example, how the ice interacts with the air above it. Our post today ...[Read More]