News from the Institute

Two sediment cores attached to a folding rule. Some darker layers stand out. Below the sediment cores is a white board labeled "Bottom" (left) and "Top" (right) as well as "M51/3 SL123", "Archive", "#580" and "Sec. 4"

Why Did the Deep-Sea Ecosystem in the Eastern Mediterranean Collapse 10,000 Years Ago?

During a dramatic climate change around 10,000 years ago, most bottom-dwelling organisms in the eastern Mediterranean Sea died. Using climate…

A hand holds a wooden thermometer with a red mercury column, displaying temperatures in degrees Celsius and Fahrenheit. The red column indicates approximately 40 °C (100 °F). In the blurred background, a building is visible under a blue sky, suggesting a hot outdoor temperature.

Climate Models With High Resolution in the Ocean Can Better Represent European Heat Waves

The North Atlantic significantly influences the weather in Europe. For instance, a cold spell in the subpolar North Atlantic can lead to a heat wave…

Image of a hurricane, visible through white cloud vortices, from above.

How Ocean Eddies Influence the Intensity of Tropical Cyclones

Depending on whether they carry warm or cold water, ocean eddies can intensify or weaken tropical cyclones. A study conducted at the Max Planck…

Map of the North Atlantic. Continents are black, and the ocean is colored with a blue-to-yellow color code.

How to Make Model Experiments on the Atlantic Overturning Circulation More Realistic

Melting ice in the Arctic is causing an increasing amount of freshwater to enter the North Atlantic, which is expected to result in a weakening of…

Young researchers stand in front of the entrance to the auditorium on the Bucerius Law School campus. A banner hangs there with the words “CELLO Conference 2025.”

CELLO: Climate Exploration in Lively Liaison with the Ocean

From September 16 to 18, 2025, around 220 ocean researchers have met at the CELLO conference organized by the Max Planck Institute for Meteorology.…

Waves on a beach at the North Sea, the sky is overcast.

Weaker Ocean Circulation Could Cost Trillions

A major motor for the global climate is beginning to falter: a massive system of ocean currents called the Atlantic Meridional Overturning…

How the Atlantic overturning got its observing system

The RAPID observing system has monitored the Atlantic Meridional Overturning Circulation (AMOC) at 26.5°N since 2004. Many physical oceanographers…

 Katabatic storm („Piteraq“) on 20. September 2003

How katabatic storms in southeast Greenland form dense water in the Irminger Sea

In a new study in the Journal of Geophysical Research: Oceans, Dr. Oliver Gutjahr (Universität Hamburg, Max Planck Institute for Meteorology (MPI-M))…

Global flow visualization in 100m depth, illustrating several eddy-rich areas around the world.

Project EERIE: Ocean eddies for better climate projections

The Max Planck Institute for Meteorology (MPI-M) is successfully involved in the new EU project EERIE (European Eddy-RIch Earth system models).…

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Abrupt CO2 quadrupling: Resolving ocean eddies leads to smaller increase in global mean surface temperature

In a recent study in Geophysical Research Letters, Dr. Dian Putrasahan and colleagues from the department “The Ocean in the Earth System” at the Max…

Ocean modelling at MPI-M – from LSG to ICON-O

The Max Planck Institute for Meteorology (MPI-M) has a long tradition of creating general circulation models of the ocean in order to pursue its…

Shifting winds weakened the recent Southern Ocean CO2 absorption

In a new study, Lydia Keppler and Dr Peter Landschützer from department “The Ocean in the Earth System” at the Max Planck Institute for Meteorology…

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