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Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research


Southern Ocean: Reconstructing environmental conditions over the past 30,000 years

Researchers reconstruct environmental conditions in the Southern Ocean over the past 30,000 years, showing that seasonal sea-ice zones had significant influences on ecosystems and carbon cycling. The study reveals that nutrient-rich waters allowed phytoplankton to store CO2, contributing to global cooling during ice ages.

Climate research: Where is the world's permafrost thawing?

The first global permafrost database has been launched, offering a comprehensive dataset on permafrost temperature and active layer thickness. The GTN-P database, compiled by an international team of researchers from 25 countries, will help scientists better understand the extent to which climate change is causing permafrost thawing.

Microplastics in the ocean: Biologists study effects on marine animals

A study by biologists at the Alfred Wegener Institute found that ingestion of microplastic particles does not mechanically affect marine isopods. In a feeding experiment, researchers offered isopods artificial food supplemented with plastic particles, which were traced through the digestive system using various microscopy techniques.

Permafrost soil: Possible source of abrupt rise in greenhouse gases at end of last Ice Age

Researchers found that thawing Arctic permafrost soil may have released large amounts of carbon dioxide and other greenhouse gases into the atmosphere around 14,600 years ago. The study suggests that this process could have amplified initial warming through positive feedback, similar to current effects of permafrost thawing in Siberia.

How variable are ocean temperatures?

A new study shows that sea surface temperatures reconstructed from climate archives vary to a much greater extent on long time scales than simulated by climate models. The researchers found that conventional climate models underestimated the variations of sea surface temperatures by a factor of 50 on a millennial time scale.

SourceAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research·JournalProceedings of the National Academy of Sciences·DateNov 10, 2014

'Like a giant elevator to the stratosphere'

A new study reveals a previously unknown atmospheric phenomenon over the South Seas, which boosts ozone depletion in polar regions and could have a significant influence on future climate. The discovery of the 'OH shield' layer allows long-lived chemical compounds to enter the stratosphere, contributing to global impact.

Long-term study reveals: The deep Greenland Sea is warming faster than the world ocean

A long-term study has revealed that the deep Greenland Sea is warming at a rate ten times higher than the global ocean, with potential consequences for European climate. The warming is caused by changes in the interplay of two processes: cooling from above and warming from below.

Stratospheric ozone chemistry plays an important role for atmospheric airflow patterns

Researchers at the Alfred Wegener Institute found that stratospheric ozone chemistry significantly influences the Arctic Oscillation, leading to changes in atmospheric air flows and temperature distribution. This basic knowledge is crucial for improving climate models and reducing uncertainty in simulated climate developments.

Ocean current links northern and southern hemisphere during Ice Age

Researchers from EPICA project establish precise link between climate records from Greenland and Antarctica using methane concentration data. They find that short temperature changes in the South are connected to fast changes in the North through Atlantic Ocean currents, indicating a general 'bipolar seesaw' connection.