Increased AMOC slowdown in high-resolution models

Scientists from the department "The Ocean in the Earth System" at the Max Planck Institute for Meteorology (MPI-M) have shown in the Journal of Advances in Modeling Earth Systems why the Atlantic Meridional Overturning Circulation (AMOC) slows down significantly when the resolution for the atmosphere in the Earth System Model of the MPI-M (MPI-ESM)...

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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 (MPI-M) find that the carbon dioxide (CO2) absorption in the Southern Ocean weakened between 2012 and 2016. The study links shifts in regional winds to this reduced carbon uptake.

Similar to a fizzy...

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Cause for variability in Arctic sea ice clarified

Using extensive computer simulations, the scientists Dr Dirk Olonscheck, Dr Thorsten Mauritsen and Dr Dirk Notz from the Max Planck Institute for Meteorology (MPI-M) in Hamburg and the University of Stockholm are now able to explain why the Arctic sea ice varies greatly from year to year. Their results were recently published in Nature Geoscience.

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Contribution to understand the long‐term response of the ocean carbon cycle to climate change

In a new study in Geophysical Research Letters Dr Tatiana Ilyina and Dr Mathias Heinze from the department "The Ocean in the Earth System" at the Max Planck Institute for Meteorology (MPI-M) found that during the Paleocene-Eocene Thermal Maximum (PETM) changes in overturning circulation are key to reproducing the deoxygenation and carbonate...

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New group at MPI-M: Observations, Analysis and Synthesis (OAS)

In May 2019 the new group "Observations, Analysis and Synthesis (OAS)", led by Dr Peter Landschützer, started in the department "The Ocean in the Earth System" at the Max Planck Institute for Meteorology (MPI-M). The group combines, extrapolates and interprets various observations of the Earth System from satellite data through shipboard data to...

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Humboldt Research Fellow Thibaut Dauhut starts working at MPI-M

Thibaut Dauhut, Ph.D., a PostDoc from the Laboratoire d'Aérologie at the Université de Toulouse, France, was selected by the Alexander von Humboldt foundation to receive a Humboldt Research Fellowship for Postdoctoral Researchers. For his 18-month stay he joins the Max Planck Institute for Meteorology (MPI-M) from 1st May 2019 on and will be...

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Minerva Fast Track and new group for Claudia Stephan

Beginning in May 2019 a new working group on cloud-wave coupling led by Dr Claudia Stephan has joined the department "The Atmosphere in the Earth System" at the Max Planck Institute for Meteorology (MPI-M). Claudia Stephan was awarded a Minerva Fast Track position by the Max Planck Society (MPG). MPI-M congratulates Claudia Stephan!

Tropical...

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New estimates of the future effect of air pollution on Earth´s radiation budget

Almost all IPCC scenarios for 2015 to 2100 show a reduction in the air pollution by anthropogenic aerosols for the future, but their effects on the radiation budget are different. Dr Stephanie Fiedler, scientist in the department "The Atmosphere in the Earth System" at the Max Planck Institute for Meteorology (MPI-M), and her co-authors come to...

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Administrative Centre for China's Agenda 21 visits MPI-M

A delegation of high-level representatives from the Administrative Centre for China's Agenda 21 (ACCA21) of the Ministry of Science and Technology of China visited the Max Planck Institute for Meteorology (MPI-M) and the German Climate Computing Centre (DKRZ) on 29th of April 2019.

The ACCA21 was established in 1994 with the mission to conduct...

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Predicting the variable CO2 uptake by the ocean

The ocean CO2 uptake is predictable for two years in advance, according to new paper in Science Advances by Dr Hongmei Li, Dr Tatiana Ilyina, Dr Wolfgang A. Müller, and Dr Peter Landschützer, all scientists in the department “The Ocean in the Earth System” at the Max Planck Institute for Meteorology (MPI-M).

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