CR
Cryospheric Sciences

Regular Author

Image of the Week – Ice Ice Bergy

May 19, 2017
Image of the Week – Ice Ice Bergy
An iceberg travelling by Greenland. [Credit: Credit: Romain Schläppy, distributed via imaggeo.egu.eu]

They come in all shapes, sizes and textures. They can be white, deep blue or brownish. Sometimes they even have penguins on them. It is time to (briefly) introduce this element of the cryosphere that has not been given much attention in this blog yet: icebergs! What is an iceberg? Let’s start with the basics. An iceberg, which literally translates as “ice mountain”, is a bit of fresh ice that brok ...[Read More]

Image of the Week – Antarctica’s Flowing Ice, Year by Year

May 12, 2017

Today’s Image of the Week shows annual ice flow velocity mosaics at 1km resolution from 2005 to 2016 for the Antarctic ice sheet. These mosaics, along with similar data for Greenland (see Fig.2), were published by Mouginot et al, (2017) last month as part of NASA’s MEaSUREs (Making Earth System Data Records for Use in Research Environments) program. How were these images constructed? The mosaics s ...[Read More]

Image of the Week – The ups and downs of sea ice!

April 7, 2017
Image of the Week – The ups and downs of sea ice!
Figure 1: Left - Mean sea-ice extent in September 2016 (month of minimum sea-ice extent) compared to the median ice edge between 1981 and 2010 (pink). Right- Mean sea-ice extent in March 2017 (month of maximum sea-ice extent) compared to the median ice edge between 1981 and 2010 (pink). [Credit: Image courtesy of the National Snow and Ice Data Center]

The reduction in Arctic sea-ice cover has been in the news a lot recently (e.g. here) – as record lows have been observed again and again within the last decade. However, it is also a topic which causes a lot of confusion as so many factors come into play. With this Image of the Week we will give you a brief overview of the ups and downs of sea ice! In general, Arctic sea ice is at its minim ...[Read More]

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

February 24, 2017
Image of the Week — The ice blue eye of the Arctic
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 – On the tip of Petermann’s (ice) tongue

January 27, 2017
Image of the Week – On the tip of Petermann’s (ice) tongue
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]

Image of the Week – For each tonne of CO2 emitted, Arctic sea ice shrinks by 3m² in summer

January 20, 2017
Image of the Week – For each tonne of CO2 emitted, Arctic sea ice shrinks by 3m² in summer
Mean area of Arctic September sea ice lost by CO2 emissions of each citizen for each country of the world in 2013. These results are based on the observed trend of 3 m² sea-ice area loss per tonne of CO2 emitted [Credit: adapted from Notz and Stroeve (2016), Fig.S1]

Declining sea ice in the Arctic is definitely one of the most iconic consequences of climate change. In a study recently published in Science, Dirk Notz and Julienne Stroeve find a linear relationship between carbon dioxide (CO2) emissions and loss of Arctic sea-ice area in summer. Our image of this week is based on these results and shows the area of September Arctic sea ice lost per inhabitant d ...[Read More]

Image of the Week — Allez Halley!

December 16, 2016

On the Brunt Ice Shelf, Antarctica, a never-observed-before migration has just begun. As the pale summer sun allows the slow ballet of the supply vessels to restart, men and machines alike must make the most of the short clement season. It is time. At last, the Halley VI research station is on the move! Halley, sixth of its name Since 1956, the British Antarctic Survey (BAS) has maintained a resea ...[Read More]

Image of the Week – What an ice hole!

November 25, 2016
Image of the Week – What an ice hole!
A schematic representation of what causes polynyas to open [Credit: Céline Heuzé]

Over the summer, I got excited… the Weddell Polynya was seemingly re-opening! ”The what?” asked my new colleagues. So today, after brief mentions in past posts, it is time to explain what a polynya is. Put it simply, a polynya, from the Russian word for “ice hole”, is a hole in the sea-ice cover. That means that in the middle of winter, the sea ice locally and naturally opens and reveals the ocean ...[Read More]

Image of the Week – Inside a Patagonian Glacier

November 4, 2016
Image of the Week – Inside a Patagonian Glacier
Figure 1: A speleologist descending inside a glacier cave of the Grey Glacier [Credit: Tommaso Santagata/ La Venta]

Chilean Patagonia hosts many of the most inhospitable glaciers on the planet – in areas of extreme rainfall and strong winds. These glaciers are also home to some of the most spectacular glacier caves on Earth, with dazzlingly blue ice and huge vertical shafts (moulins). These caves give us access to the heart of the glaciers and provide an opportunity to study the microbiology and water drainage ...[Read More]

Image of the Week — FRISP 2016

October 7, 2016
Image of the Week — FRISP 2016
Group picture of the FRISP 2016 meeting [Credit: Anna Wåhlin]

The Forum for Research into Ice Shelf Processes, aka FRISP, is an international meeting bringing together glaciologists and oceanographers. There are no parallel sessions; everyone attends everyone else’s talk and comment on their results, and the numerous breaks and long dinners encourage new and interdisciplinary collaborations. In fact, each year, a few presentations are the result of a previou ...[Read More]