Polar Talk #21 – Save the Date
Am 06.05.2026 um 18:30 Uhr findet der #21 Polar Talk im Naturhistorischen Museum Wien statt. Nirgends verliert die Erde so viel Energie wie in den Polargebieten. Sie kühlen damit nicht nur sich selbst sondern auch den Planeten insgesamt, aber gerade…
The Hunga Tonga eruption continues to have an impact on weather patterns
GOES-17 visible-band snapshot of the Hunga Tonga–Hunga Ha'apai eruption on 15 Jan 2022 (04:30 UTC). The key point: the plume rose unusually high into the stratosphere, helping loft water vapour that can influence climate for years.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 A broad view of…
In the Shadow of Climate Change – What Remains of the “Eternal Ice”?
Figure: The Mittivakkat Glacier shown here is located near the Sermilik research station in East Greenland. (© Karl Steinegger 2024) The majority of the world’s freshwater is stored in glaciers and ice sheets. If all of Earth’s ice were formed…
Focus on glaciers: Review of the activities of the Austrian Polar Research Institute in the Year of Glacier Preservation
Research Expedition to the Sermilik Station: How Eduard Orel’s Great-Great-Grandson is Learning Polar Research
Behind the Scenes – A transdisciplinary, comparative analysis reveals key risks from Arctic permafrost thaw
The discovery of Franz Josef Land 150 years ago and its Impact on International Polar Research – Part 2
