Cryospheric Sciences

Image of the Week – Blood Falls!

Emma C. Smith December 9, 2016

Blood Falls, Antarctica. Red coloured water emerges from the front of Taylor Glacier. For scale - the tent at the left of the image is around 4 m long. [Credit: Peter Rejcek , NSF]

If glaciers could speak, you might imagine them saying – “HELP!” The planet continues to warm and this means glaciers continue to shrink. Our new image of the week shows a glacier that appears to be making this point in a rather dramatic and gruesome way – it appears to be bleeding! If you went to the snout of Taylor Glacier in Antarctica’s Dry Valley region (see map ...[Read More]

Ice-Hot News : The “Oldest Ice” quest has begun

Oldest Ice PhD Students November 14, 2016

There is million-year old ice somewhere deep under the surface of the Antarctic ice sheet! [Credit: Brice Van Liefferinge]

This is it! The new European horizon 2020 project on Oldest Ice has been launched and the teams are already heading out to the field, but what does “Old Ice” really mean? Where can we find it and why should we even care? This is what we (Marie, Olivier and Brice) will try to explain somewhat. Why do we care about old ice, ice cores and past climate? Unravelling past climate and how it responded to ...[Read More]

Image of The Week – 100 years of Endurance!

Emma C. Smith August 26, 2016

Shakleton's Endurance finally sinks to the bottom of the Weddell sea in November 1915. [Credit: Royal Geographical Society via Wikimedia Commons]

The 30th August 2016 marks 100 years since the successful rescue of all (human) member of Shackleton’s Endurance crew from their temporary camp on Elephant Island (see map). Nearly a year prior to their rescue they were forced to abandon their ship – The Endurance – after it became stuck in thick drifting sea ice, known as pack ice, trying to navigate the Weddell Sea. It was the last major e ...[Read More]

Image of the Week — Where do people stay in the “coolest” place on earth?

Sophie Berger August 19, 2016

The 82 research stations in the Antarctic. The world map below shows which countries are operating a station in Antarctica. Source: COMNAP Antarctic Facilities (Updated February 2014) - [Credit: Sophie Berger]. Click here here to enlarge the image.

What word would you use to characterise the Antarctic ? White? Windy? Remote? Empty? Inhospitable? Wild? Preserved? While all of these are true it may surprise you to find out that the Antarctic is occupied by humans all year round with almost half of its 82 research stations operating 365.25 days a year! Just a few hours before the launch of the biennial Antarctic meeting held by the Science Comm ...[Read More]

Image of the week – The winds of summer (and surface fluxes of winter)

Céline Heuzé July 22, 2016

Representation of the (a) summer and (b) winter oceanic circulation within the Adélie region, East Antarctica. MGT = Mertz Glacier Tongue (red dot on the Antarctica map); other acronyms indicate different water masses: Antarctic Surface Waters (AASW), Modified Circumpolar Deep Water (MCDW*), Dense Shelf Water (DSW) and Antarctic Bottom Water (AABW) explained below. [Credit: reprinted with permission from Snow et al. (2016, figure 4) ]. Click here here to enlarge the image.

Antarctica is separated from the deep Southern Ocean by a shallow continental shelf. Waters are exchanged between the deep ocean and the shallow shelf, forming the Antarctic cross-shelf circulation: Very dense waters leave the shelf as Antarctic Bottom Water (AABW) that will then flow at the bottom of all oceans. Meanwhile, relatively warm water from the Southern Ocean, Modified Circumpolar Deep W ...[Read More]

Image of the Week – How ocean tides affect ice flow

Teresa Kyrke-Smith July 8, 2016

(a) Shaded relief map of Rutford Ice Stream (West Antarctica) and surrounding area. Red box indicates the region shown in b. (b) Horizontal velocity where colors indicate speed, arrows show flow direction, and grayscale background is horizontal speed from Rignot et al. (2011). (c) Detrended along-flow displacements measured with GPS stations beginning December 2003. Locations of stations are indicated in (b). ( Credit : Brent Minchew )

Ice streams discharge approximately 90% of the Antarctic ice onto ice shelves , and ultimately into the sea into the sea (Bamber et al., 2000; Rignot et al., 2011). Whilst flow-speed changes on annual timescales are frequently discussed, we consider here what happens on much shorter timescales! Previous studies have shown that ice streams can respond to ocean tides at distances up to 100km inland ...[Read More]

Marine Ice Sheet Instability “For Dummies”

David Docquier June 22, 2016

MISI is a term that is often thrown into dicussions and papers which talk about the contribution of Antarctica to sea-level rise but what does it actually mean and why do we care about it? MISI stands for Marine Ice Sheet Instability. In this article, we are going to attempt to explain this term to you and also show you why it is so important. Background The Antarctic Ice Sheet represents the larg ...[Read More]

An Antarctic Road Trip

Nanna B. Karlsson June 8, 2016

Arriving at our first drill site with our sledge containing drill equipment, survival box and of course our lunch. Credit: N. B. Karlsson

Working in the Arctic and Antarctic presents its own challenges. It is perhaps easy to imagine how a station situated close to the coast is resupplied: during the summer, one or more ships will arrive bringing fuel, food and equipment, but what about stations inland? Flying in supplies by aircraft is expensive and, in the case of large quantities of fuel, unsustainable. Besides, many stations are ...[Read More]

Image of the Week – Storing water in Antarctica to delay sea-level rise

David Docquier April 29, 2016

Difference in ice thickness from the initial equilibrium state after 100 years of ice addition (upper panels) and 1000 years after the end of the forcing (lower panels). Two scenarios are shown, 200 km (left panels) and 800 km (right panels) from the coastline, both corresponding to a sea-level mitigation of 10 mm per year (credit: Frieler et al., 2016, fig 3) .

Sea level rise Sea-level rise is one of the main impacts of the current global warming and its rate has dramatically increased in the last decades (the current rate is about 3 mm per year). Even if greenhouse gas emissions were stopped today, sea level would continue to rise due to the slow Earth climate system response (IPCC, 2013, chap. 13). It is therefore a considerable threat for popul ...[Read More]

Image of the Week: The Bipolar Seesaw

Nanna B. Karlsson April 8, 2016

Ice core records from the WAIS core showing fast millennial-scale climatic variability. Reprinted by permission from Macmillan (Publishers Ltd: Nature, WAIS Divide Project Members, 2015, vol. 520).

The colourful graphs above show how the climate changed in the period from 65 to 25 thousand years ago when Earth was experiencing an ice age. A wealth of information on the dynamics of our climate is embedded in the curves, especially how the northern and southern hemisphere interact, and how fast climate can change. The figure represents thousands and thousands of hours of work by scientists, te ...[Read More]