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Photo taken by the above-ice camera at ice station 1 in the Atlantic sector of the northern Fram Strait.

The influence of natural climate variability

The sea-ice minimum in the Arctic wasn’t as low as expected. The explanation: natural fluctuations in the climate system, which are becoming increasingly important.

Polar 6 flies over Regime 3 during work on the ice, 22 July 2025

How the Arctic Sea Ice Melted in Summer 2025

CONTRASTS expedition has successfully observed the summer 2025 sea-ice melting in detail; now the analysis of the data and samples begins.

A Wake-Up Call from Antarctica

A new study presents evidence of an abrupt shift in the Antarctic climate system. The dramatic decline in sea ice plays a key role.

Screenshot of the MapViewer on board the Polarstern.

Satellites as Guides for RV Polarstern

The digital map system “Mapviewer” is essential for route planning and navigation through sea ice and is evaluated during the CONTRASTS expedition.

A hyperspectral camera (black box on tripod) measuring the reflectivity of a meltpond.

Midsummer in the Arctic

Most of this year’s young sea ice has now melted.

Broadband albedo measurements and ASD spectral albedo measurements

Where does the sunlight go?

Sea ice and sunlight: fascinating and essential components of the Arctic summer

At Station 1, parts of the ice cover were melted to such an extent that the darker ocean could be seen through the ice.

Up to 40-centimetre drop in thickness within two weeks

In the Arctic, participants in the Polarstern expedition CONTRASTS observed the rapid melting of the one- and two-year-old ice in July

ROSINA is returned to the deck after capturing images of phytoplankton, zooplankton, fish, jellies, and settling particles.

How does sea-ice melting impact the ecosystem?

The three CONTRASTS sea ice regimes exhibit major differences in terms of their ecosystems – from the sea ice to the deep sea.

Is the ocean melting the sea ice?

CONTRASTS investigates possible ocean regimes and how they influence the melting of sea ice.

The 10-metre-high weather mast (left) and the energy balance station (right).

Where the atmosphere touches the sea ice

Sea-ice melting depends to a great extent on weather conditions. Significant differences are also expected between regions.