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Investigating glaciers in depth
by Staff Writers
Nuremberg, Germany (SPX) Oct 25, 2018

File image of an ice field on Svalbard island.

Global sea level is rising constantly. One factor contributing to this rise is the melting of the glaciers. However, although the surface area of the glaciers has been well mapped, there is often no information regarding their thickness, making it impossible to calculate their volume.

As a result, we cannot accurately calculate the effects on sea levels. Dr. Johannes Furst from the Institute of Geography at Friedrich-Alexander-Universitat Erlangen-Nurnberg (FAU) has developed an approach which can be used to draw up regional ice thickness maps for glaciers. He has now produced such a map for Svalbard and published his findings in Geophysical Research Letters (DOI: 10.1029/2018GL079734).

New ice thickness map, new findings
The FAU geographer Johannes Furst has gathered and evaluated data measured by a number of international research teams since the early 1980s. These measurements have been entered into the new map of glacier thickness on Svalbard, an archipelago to the north of Norway with the main island Spitsbergen.

Whereas previous studies have only looked at individual thickness measurements in isolation, projecting the total ice volume evolution on the basis of the surface area and just a few measurements, this map takes all available measurements into account in order to obtain a reliable estimate of the total ice volume.

At 6,200 cubic kilometres, it is approximately one third smaller than previously presumed. Nevertheless, if this ice were to melt all of a sudden, it would still cause global sea levels to rise by 1.5 centimetres.

Furst also provides an associated map of error estimates. Errors may be a direct result of the thickness measurements. At these locations, errors can readily be calculated. It is more difficult for positions away from the measurements.

Starting from a certain measurement point, errors are estimated along flowline down the glacier based on speed, direction as well as local mass gain and loss. Researchers could also use this formula to calculate the ice thickness uncertainty for regions where hardly any measurements have been taken.

'In order to calculate the future demise of glaciers accurately, we have to know the thickness of the glaciers. Until now, however, we have only had very rough estimates, which vary greatly. This is down to the lack of measurements taken worldwide. My approach, which can also be used for other glaciers, may help in this respect,' Johannes Furst explains.

Data, data, data
There are nearly 1,700 glaciers on Svalbard. On these, one million point measurements of the ice thickness have already been collected, ranging in date from the 1980s to the present day.

These measurements have mainly been provided by British, Spanish, Norwegian and Danish teams of researchers, but Polish, Icelandic, French and Japanese researchers have also collected valuable data. One method of determining the thickness of the ice cap is using radar. A radar signal is sent down through the ice. The longer the signal takes to return to the measuring device, the thicker the ice is.

'It's like ping-pong: the table tennis player hits the ball and waits until it comes back. The longer he has to wait, the further away the ball was,' explains Furst. Another method involves making several boreholes through several hundred metres of ice.

The extracted ice cores were used, for example, to study past fluctuations in temperature or precipitation. A mining company has also used drilling in order to better judge the risks of mining for coal underneath the glacier. Furst has included all these measurements in the ice thickness map.

Going with the flow
The ice thickness map gives new insights into the dynamic ice loss of glaciers. When new snow falls, its weight compresses previous layers of snow and a new mass of ice is gradually formed. This ice then flows downglacier, in some places until it reaches the ocean.

Huge icebergs regularly break off from the ice cliffs there. The mass lost there every year can only be estimated accurately if you know how thick the ice at the ice cliffs actually is. Johannes Furst has calculated an average thickness of 135 metres for all marine-terminating glaciers in the Svalbard archipelago. The previous estimate was 214 metres. Thanks to the new map, we are now able to accurately estimate the dynamic ice loss from Svalbard glaciers.

Research paper


Related Links
University of Erlangen-Nuremberg
Beyond the Ice Age


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ICE WORLD
Scientists find missing piece in glacier melt predictions
Stanford CA (SPX) Oct 17, 2018
Stanford scientists have revealed the presence of water stored within a glacier in Greenland, where the rapidly changing ice sheet is a major contributor to the sea-level rise North America will experience in the next 100 years. This observation - which came out of a new way of looking at existing data - has been a missing component for models aiming to predict how melting glaciers will impact the planet. The group made the discovery looking at data intended to reveal the changing shape of Store G ... read more

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