News from the Institute

Aerial view of a massive glacier in a snow-covered mountain landscape. The glacier flows through the mountains and shows characteristic features such as meltwater streams and crevasses. The surrounding mountains are partially rocky and snow-covered, while the sun casts long shadows and highlights the texture of the ice.

Stability of the Greenland Ice Sheet: When the Ice Loss Becomes Irreversible

In a pre-industrial climate, the Greenland Ice Sheet can take on four different steady states, as demonstrated by simulations using a fully-coupled…

Photo of massive icebergs in Antarctica in front of a clear blue sky.

Study Reveals Previously Unknown Teleconnection Between Northern Hemisphere Ice Sheets and West Antarctica

Changes in the Northern Hemisphere ice sheets can propagate through the climate system and affect even the remote region of Antarctica. Idealized…

New Climate Model Reveals the Triggers of Abrupt Climatic Changes in the Past 20,000 Years

Between the last glacial maximum and today, humans were exposed to severe changes of the climate: Coastal settlement areas were lost due to rising…

A new mechanism for synchronising Heinrich events with Dansgaard-Oeschger cycles

The northern hemisphere climate during the last glacial period (about 65,000-15,000 years before present) was dominated by two prominent signals of…

Graphic of the iceberg meltwater flow in the Atlantic

Including icebergs in computer models helps to better understand past climate change

In their new study Olga Erokhina and Uwe Mikolajewicz showed that adding icebergs to climate models can help scientists better understand the…

Focus: The big melt | Marie-Luise Kapsch, Clemens Schannwell

Climate change is melting the ice sheets of Greenland and Antarctica and causing sea levels to rise. This could be a disaster for island states and…

Figure of ice shelf

How ice rises and rumples affect the Antarctic ice sheet

In a study in The Cryosphere, researchers at the Max Planck Institute for Meteorology examined the effect of basal friction and sea level variation…