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New satellite technology promises great progress for glacier research

Researchers are developing a unique radar, which could allow a view of Earth’s ice sheets
Das Forschungsflugzeug Polar 6 fliegt über einen Schmelzwasser-See auf dem 79-Grad-Nord-Gletscher im Nordosten Grönlands.
Research aircraft Polar 6 flies over a supraglacial lake on the 79-degree north glacier in the north-east of Greenland. (Photo: Alfred-Wegener-Institut / IceCam)

Scientists from the Alfred Wegener Institute are developing with experts from the German Aerospace Centre (DLR) a new satellite measurement method for the observation from space of the large ice masses of Greenland and the Antarctic. “Tandem-L” is the name of a new satellite radar system, which launched in the year 2022 could provide urgently needed data concerning the shrinkage of the ice sheets in both hemispheres. Concerning the construction of the radar and the launch of the satellite mission of the same name, the Science Council is to advise the Federal Ministry of Education and Research (BMBF) at the end of November as part of a review procedure.

"Extreme" is the word glaciologists now use to describe the extent of the annual summer melt on the surface of the Greenland ice sheet. This year, the scientists observed, especially in the north-east of Greenland, a widespread network of supraglacial lakes and streams on the ice sheet. Their water masses give cause for concern, above all for one reason: The melt water almost always makes its way through the ice sheet. At the ice base this water acts like a lubricant. It increases the speed at which the glaciers move. The result: Larger ice masses slip into the ocean; the sea level rises to a greater extent.

In order to be able to investigate the effects of surface melt on the glaciers and ice sheets of the world more profoundly and, above all, in large areas, scientists from the Alfred Wegener Institute have been assisting experts from the German Aerospace Centre over the past four years to create a new, satellite-based radar concept. This detects the changes in the ice sheets for the first time using a tomographic method and, for example, makes the penetration of the melt water visible.

"The new Tandem-L radar operates in the so-called L-band range. It emits radio waves with a wavelength of 24 centimetres, which in contrast to the previous satellite technology penetrate up to 100 metres deep in ice and snow. Thus, glaciologists would have the first opportunity to extensively screen the topmost ice layer of the glaciers and ice sheets from space and to map their inner structure. In addition, we can also measure the changes in the glacier surface with Tandem-L”, says Professor Angelika Humbert, Head of the Glaciology Section at the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI).

For the Tandem-L mission, she and her team had initially analysed data from the already operating satellites TerraSAR-X and TanDEM-X. On the basis of this, they were able to develop methods of analysis and filtration that could be used to understand the origin of the structures in the Tandem-L images and to use the data for ice modelling.

To date, glaciologists have used aircraft or satellite-based altimeters to measure the topography of the ice surface in Greenland and the Antarctic and to calculate the ice losses of ice sheets by means of the differences in altitude. Altimeters scan the surface with the aid of lasers or radar. It is important that the waves emitted by the satellites do not penetrate the ice surface. The new Tandem-L system, on the other hand, will look deep into the ice and allow scientists to gain completely new insights with its high-resolution L-band data.

The satellite mission Tandem-L consists of two satellites, each of which is equipped with an L-band radar and are to orbit around the Earth in formation at an altitude of 760 kilometres. The radars scan the Earth's surface with a strip 175 to 350 kilometres wide. "Tandem-L will not only provide us with important ice information, but also receive urgently needed data on global forest biomass, soil moisture and ocean currents", says the scientific coordinator of the satellite mission Professor Irena Hajnsek from the Microwaves and Radar Institute at DLR.

At the beginning of this year, the BMBF launched an assessment procedure for the development of a roadmap for research infrastructures in Germany. Within the scope of this, the Scientific Council meets at the end of this month and, among other things, advises on the Tandem-L mission. The results of the assessment are expected for mid-2017.

Please find further information at the following websites:http://www.dlr.de/HR

Contact

Your scientific contact persons at the DLR are:

Prof. Dr.-Ing. Alberto Moreira (tel.: +49 8153 28-2306; e-mail: Alberto.Moreira(at)dlr.de)
Prof. Dr. rer. nat. Irena Hajnsek (tel.: +49 8153 28-2363 ; e-mail: Irena.Hajnsek(at)dlr.de)

Your contact person in the DLR Press Office is Elisabeth Schreier (tel.: +49 8153 28-1787; e-mail: Elisabeth.Schreier(at)dlr.de)

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Das Forschungsflugzeug Polar 6 fliegt über einen Schmelzwasser-See auf dem 79-Grad-Nord-Gletscher im Nordosten Grönlands.
Research aircraft Polar 6 flies over a supraglacial lake on the 79-degree north glacier in the north-east of Greenland. (Photo: Alfred-Wegener-Institut / IceCam)
Die zwei Tandem-L-Satelliten mit großen entfaltbaren Reflektorantennen im Formationsflug. Tandem-L ist ein Vorschlag für eine hochinnovative Satellitenmission zur globalen Beobachtung von dynamischen Prozessen auf der Erdoberfläche in einer bisher nicht erreichten Qualität und Auflösung. Aufgrund seiner neuartigen Abbildungstechniken und seiner enormen Aufnahmekapazität wird Tandem-L dringend benötigte Informationen zur Lösung hochaktueller wissenschaftlicher Fragestellungen aus den Bereichen der Bio-, Geo-, Kryo- und Hydrosphäre liefern.
The Tandem-L satellites with large unfurlable reflector antennas in formation flight (Graphic: Alfred Wegener Institute / DLR)
Ein Schmelzwassersee auf dem grönländischen Eisschild. Dieses Bild entstand mit der zum Erdboden gerichteten Bordkamera des Polarforschungsflugzeuges Polar 6. Foto: Alfred-Wegener-Institut/IceCam
A supraglacial lake on the Greenland ice sheet (picture taken by IceCam, mounted on the research aircraft Polar 6) (Photo: Alfred-Wegener-Institut / IceCam)
Ein Glaziologe arbeitet direkt neben einem  Schmelzwasserbach auf dem Store-Gletscher in Westgrönland.
A glaciologist works right next to a supraglacial lake on the Store glacier (West Greenland). (Photo: Alfred-Wegener-Institut / Coen Hofstede)
Ein Schmelzwassersee auf dem Store-Gletscher in Westgrönland.
A supraglacial lake on the Store glacier (West Greenland) (Photo: Alfred-Wegener-Institut / Coen Hofstede)
Zwei Wissenschaftler des Alfred-Wegener-Institutes untersuchen in einem gefrästen Schneeschacht die Struktur und Dichte der obersten Schneeschichten des Antarktischen Eisschildes. Die Aufnahme entstand an der vom AWI betriebenen Sommer-Forschungsbasis Kohnen.
Two scientists from the Alfred Wegener Institute are investigating the structure and density of the top snow layers of the Antarctic ice sheet (picture was taken near the Kohnen summer station, operated by the AWI). (Photo: Alfred-Wegener-Institut / Martin Leonhardt)
Wissenschaftler des Alfred-Wegener-Institutes untersuchen in einem gefrästen Schneeschacht die Struktur und Dichte der obersten Schneeschichten des Antarktischen Eisschildes. Die Aufnahme entstand an der vom AWI betriebenen Sommer-Forschungsbasis Kohnen.
Two scientists from the Alfred Wegener Institute are investigating the structure and density of the top snow layers of the Antarctic ice sheet (picture was taken near the Kohnen summer station, operated by the AWI). (Photo: Alfred-Wegener-Institut / Thomas Laepple)
Diese Grafik zeigt eine tomografische L-Band-Radaraufnahme der obersten Schnee- und Firnschichten eines Gletschers. Der Untersuchungsfokus in diesem Gletscherquerschnitt liegt auf der Struktur und Dichte der Gletscheroberfläche. Je heller die Farbe ist, desto dichter ist an dieser Stelle der Schnee.
This graph shows a tomographic L-band radar image of the top snow and firn layers of a glacier. (Graphic: Alfred Wegener Institute / DLR/Matteo Pardini, Giuseppe Parrella)
Diese Grafik zeigt eine tomografische  L-Band-Radaraufnahme der obersten Schnee- und Firnschichten eines Gletschers. Der Untersuchungsfokus in diesem  Gletscherquerschnitt liegt auf den Dichte- und Strukturunterschieden. Das heißt, je heller die Farbe ist, desto dichter sind an diesen Stellen die Schnee- und Firnschichten. 
In dieser Abbildung konnten die Wissenschaftler zwei verschiedene Eistypen identifizieren – Typ 1 mit den sehr gut sichtbaren Schichten in einer Tiefe von 20 bis 40 Metern und Typ 2 mit seinen Schichten zwischen 0 und 30 Metern.
This graph shows a tomographic L-band radar image of the top snow and firn layers of a glacier. (Graphic: Alfred Wegener Institute / DLR/Matteo Pardini, Giuseppe Parrella)
Flyer Tandem-L (pdf file)
Photo Credits (in German)

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