Skip to main content

Calving Glacier in Greenland

Credits
USGS; Link: http://earthexplorer.usgs.gov/

In this image you can see a glacier (blue) in Greenland calving into the sea (black). The glacier is surrounded by landmass, indicated by the red colour in the upper and the lower part of the picture. In recent years, hardly any place on earth has been more affected by climate warming than the Arctic: The ice along the edge of the giant ice cap is getting thinner and thinner, and glaciers are calving more and more rapidly. It remains to be seen if increasing snowfalls on the inner landmass can make up for the loss of frozen material at the edge of the ice cap.

 

Volcanic Ash of des Eyjafjallajökull, Iceland

Credits
NASA/GSFC; Link: http://rapidfire.sci.gsfc.nasa.gov

Iceland is located in the geologically active zone where the outer mantle of the Earth is drifting apart (diverging lithosphere), and is placed on the Mid-Atlantic Ridge. Here, many active vulcanoes are covered with snow due to the cold climate. In 2010, the eruption of the glaciated vulcano Eyjafjallajökull caused an enormous ash cloud moving south which can be seen in the picture. This cloud brought all air traffic in Europe to a standstill for several days and caused high economic loss.

 

Location: Iceland

Picture taken on May 11, 2010

Sensor: MODIS Terra

Mertz Glacier and Icebergs

Credits
NASA (Jesse Allen); Link: http://earthobservatory.nasa.gov

With its ice tongue pointing towards Australia and New Zealand, the Mertz Glacier in East Antarctica extends into the Southern Ocean. A glacier can “calve”, which means that pieces of ice break off and start to float in the open sea as icebergs. Often comprising an area of several square kilometres, sea currents make these giants cross the Antarctic for months or even years. However, as soon as they reach northern and warmer areas, they begin to melt.

 

Location: Mertz Glacier, East Antarctica
Picture taken on January 1, 2010
Sensor: EO-1 - ALI

 

Glacier in Alaska

Credits
USGS; Link: http://www.usgs.gov

In the middle of this false-colour image, you can see the tongue of the Malaspina glacier. The glacier makes its way from the mountains in the north and is separated from the sea by its terminal moraine as can be seen in the lower part of the picture. Without the moraine or in the case of a sea-level rise, the glacier would come in contact with the warmer sea water and it would retreat more quickly than it does now. Satellite images and measurements on the ground show that most glaciers in Alaska are getting thinner and that only a few dozen are gaining in ice mass.

 

Hudson Bay, Canada

Credits
USGS; Link: http://earthexplorer.usgs.gov/

This image shows the two twin islands in the southern part of Hudson Bay (North and South Twin Island). In spring, the ice of Hudson Bay clears, usually leaving the south-western part, in which the two islands are located, as the last area with a closed ice sheet. Climatologists are worried about Arctic melting processes: In recent years, there have been more and more ice-free phases, signalling an increase in climate warming.

 

Location: Hudson Bay, Canada
Picture taken on February 20, 2002
Sensor: Landsat ETM+
Band combination: MIR/NIR

Glacier in Patagonia

Credits
NASA/GSFC; Link: http://visibleearth.nasa.gov

Patagonia is a mountainous region at the border between Chile and Argentina. You can see that the glacier (white) streaming from the mountains towards the foothills is interspersed with crevasses. The semicircular crest far left in the picture is pierced by three glacial rivers. The crest consists of coarse gravel, forming the terminal moraine for a long time, deposited by the ice tongue. Thus, the moraine marks the end of the glacier in former times and indicates a retreat of ice. In this false colour image, the vegetation is depicted in red.

 

Gletscher in der Antarktis

Credits
NASA (Jesse Allen, Robert Simmon); Link: http://earthobservatory.nasa.gov

The Matusevich Glacier in the Antarctic streams towards the east coast while pushing its way through a valley in the mountains. Its ice tongue has been constrained so far but once it reaches the end of the mountains, the ice spreads out and calves into the ocean. Afterwards, the undulations of the sea break the ice into small pieces that begin to flow into the open sea as icebergs.

 

Location: Antarctic

Picture taken on September 6, 2010

Sensor: EO-1 – ALI

 

Susitna Glacier in Alaska

Credits
NASA/GSFC (Jesse Allen, Robert Simmon)

In this false colour image, the Susitna Glacier in Alaska seems like a river fed by its influent streams and flowing towards the valley. Due to the depiction in false colour, the vegetation in this picture is bright red, the pure surface of the ice is light blue and white, ice covered with sediment (medial and lateral moraines) is brown and water is dark blue. The dynamics of the glacier are most striking in the middle of the picture where you can see a tributary glacier pushing its ice masses sideways into the trunk glacier.

 

Location: Alaska