Cryospheric Sciences

Careers at the European Space Agency – How and Why?

Anna Maria Trofaier & Anna Hogg May 3, 2016

Flow speed of Jakobshavn Isbræ outlet glacier (South West Greenland) in winter 2014. Credit: ESA

As the pace of modern life speeds up and job competition becomes even more fierce, it is good to have a focused plan of where you would like to be in the future. The European Space Agency (ESA) offers traineeships and research positions to young scientists on a regular basis. They may be a springboard into your chosen career path, but how do you go about bagging one of these valuable opportunities ...[Read More]

Image of the Week — Last Glacial Maximum in Europe

Sophie Berger March 4, 2016

Last glaciation in Europe, ~70,000-20,000 year BP (credit: Wikimedia Commons user Ulamm)

During the last ice age*, ~70,000 to 20,000 years ago, the climate was much colder in Europe. As a result, the northern part of Europe was fully covered by the Fennoscandian (a.k.a the Scandinavian ) ice sheet, which extended up to the British Isles and some parts of Poland and Germany. In central Europe, the Alps were also almost fully glaciated. The storage of all this ice on the continent lower ...[Read More]

Image of the Week – Changes in the Greenland Ice Sheet Documented by Satellite

Emma C. Smith February 19, 2016

Changes in mass of the Greenland Ice Sheet over 10 years from GRACE satelite data (Luthcke et al., 2013).

Monitoring the changing ice mass of the Greenland Ice Sheet provides valuable information about how the ice sheet is responding to changing climate, but how do we make these measurements over such a large area of ice? Using NASA’s GRACE satellites (twin-satellites flying in formation) it is possible to make detailed measurements of the Earth’s gravitational field. As ice is gained/lost from ...[Read More]

Image of the Week — Greenland ice sheet and clouds

Sophie Berger January 15, 2016

The effects of clouds on the Surface Mass Balance (SMB) of the Greenland ice sheet during the period September 2007–September 2010. (Credit: Van Tricht et al, 2016)

A new study combining satellite observations and model simulations shows that clouds increase meltwater runoff in Greenland by one-third compared to a cloud-free scenario. Precipitation effects not considered, clouds above the Greenland ice sheet reduce its Surface Mass Balance (SMB) [red in figure] compared to clear-sky conditions [blue in figure]. Because clouds trap the outgoing radiation from ...[Read More]

Image of the Week: Ice Sheets in the Climate

Nanna B. Karlsson December 11, 2015

The interaction of ice sheets with the atmosphere and the ocean. Excerpt from Figure 1 in Box 5.2, IPCC AR5.

Ice sheets play a central role in the climate system. They store significant amounts of fresh water and are the conveyor belts for transporting snow that accumulates on land back into the oceans. The figure above shows a few of the ice-climate interactions. In the figure below (click on the figure for full resolution) we see the complete picture of the processes taking place between ice sheets, so ...[Read More]

Image of the Week — Ice Sheets and Sea Level Rise (from IPCC)

Sophie Berger November 27, 2015

(Upper) Distribution of ice loss determined from Gravity Recovery and Climate Experiment (GRACE) time-variable gravity for (a) Antarctica and (b) Greenland, shown in centimetres of water per year (cm of water yr –1 ) for the period 2003–2012. (Lower) The assessment of the total loss of ice from glaciers and ice sheets in terms of mass (Gt) and sea level equivalent (mm). The contribution from glaciers excludes those on the periphery of the ice sheets. (Credit: IPCC (2013), Assessment Report 5, Working Group I, Technical Summary , Figure TS.3, p41)

Context On the eve of the COP21, it is of paramount importance to recall how strongly the cryosphere is affected by Climate Change. Today, we present the impact of melting ice on sea level rise, as it is presented in the latest assessment report of the Intergovernmental Panel on Climate Change. Quick facts -Since 1992, the Glaciers, Greenland and Antarctic Ice Sheets have risen the sea level by 14 ...[Read More]

Image of Week: Inside the Greenland Ice Sheet

Nanna B. Karlsson October 23, 2015

Cross-section of the age of the Greenland Ice Sheet from radar data. Credit: NASA's Scientific Visualization Studio and MacGregor et al., 2015.

The image shows a cross section of the Greenland Ice Sheet, where a recent study by MacGregor et al. have mapped the layers imaged by radar. Thanks to ice core measurements the age of the layers have been determined, and in the image the layers from the Holocene period (the past 11.700 years) are shown in green. The ice formed during the last ice age, that spanned 11.700 to 115.000 years ago are c ...[Read More]

Riding the Storm: The Arctic Circle Traverse 2015

Babis Charalampidis October 8, 2015

Stormy day at Dye-2, 20th of May. Credit: Babis Charalampidis.

In the morning on the 19th of May, we – the Arctic Circle Traverse 2015 – found ourselves in a great dilemma; to stay or to go? On our check-in conversation with the KISS crew, we were informed that an east front from Kulusuk was expected to hit our location up on the ice sheet sometime in the afternoon. The relatively low winds that we were experiencing would get stronger, and the visibility woul ...[Read More]

Image of the Week : SAFIRE team getting ready to drill in Greenland

Sophie Berger October 2, 2015

The SAFIRE team sets up the drilling device on the Store Glacier, Western Greenland. Credit : T.J. Young

How do you get a hot water drill onto an ice sheet? The Subglacial Access and Fast Ice Research Experiment (SAFIRE) uses a hot water drill to directly access and observe the physical and geothermal properties where the ice meets rock or sediment at the glacier-bed interface. Here, SAFIRE principal investigator Bryn Hubbard and post-doc Sam Doyle help fly in the drill spool at the start of the Summ ...[Read More]

Karthaus Summer School 2015

Isabel Nias September 29, 2015

The 15th Karthaus Summer School (Credit: C. Reijmer)

After a train, the London Underground, another train, a flight, three more trains and a taxi (shared with people I had met on my way); I had arrived in a small Alpine village in the very north of Italy. The reason for this rather convoluted journey? To attend the Karthaus Summer School on ice sheets and glaciers in the climate system. I’m pleased to say it was definitely worth the trip getting the ...[Read More]