2025-12-11
Professorship in the field of Polar Marine Geology and Palaeoclimatology/Palaeoceanography
The following position is to be filled in the Faculty of Geosciences
A Professorship (f/m/d) salary group W3 for the field of Polar Marine Geology and Palaeoclimatology/Palaeoceanography. The application has been prolonged to 12 January 2026. Detailed information in German and English can be found on the website of the University of Bremen:
https://www.uni-bremen.de/en/university/the-university-as-an-emplo
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https://www.uni-bremen.de/en/university/the-university-as-an-emplo
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2025-12-10
Coasts- Beaches - Shorelines
An interdisciplinary Lecture Series in the Research Focus Area Ocean Sciences, Polar Sciences and Climate Sciences
Winter term 2025/26 on select dates, Wednesdays, 6:15–7:45 p.m., Cartesium (Blue Rotunda), Enrique-Schmidt-Str. 5.
This lecture series examines aspects of coasts, beaches, and shorelines from the perspective of various disciplines, thus facilitating interdisciplinary dialogue. What happens when different cultures, people, beings, elements, materials, and forces encounter each other in littoral spaces?
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This lecture series examines aspects of coasts, beaches, and shorelines from the perspective of various disciplines, thus facilitating interdisciplinary dialogue. What happens when different cultures, people, beings, elements, materials, and forces encounter each other in littoral spaces?
more »
2025-12-08
Professorship for the subject area Marine Seismics
The following position is to be filled in the Faculty of Geosciences
A Professorship (f/m/d) salary group W2/W3 for the subject area Marine Seismics. The application deadline is 07 January 2026. Detailed information in German and English can be found on the website of the University of Bremen:
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2025-12-04
FirnMelt - Greenland’s Melting Firn and Ice Sheet Response
ERC Synergy Project approved for Angelika Humbert
The melting of the Greenland Ice Sheet is altering the porous firn layer at the glacier surface, significantly reducing its ability to retain water. As a result, increasing amounts of meltwater reach the base of the glaciers, where it influences glacier sliding and subglacial water drains into the fjords.
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