289.

How close are we to 1.5 °C or 2 °C of global warming?

 
Graphic global warming In a publication in Weather, a journal of the Royal Meteorological Society, Prof. Jochem Marotzke (Max Planck Institute for Meteorology), Dr. Sebastian Milinski (currently NCAR, Boulder, USA) and Dr. Chris Jones of the Met Office, UK, answer questions about global warming  
290.

The first version of the ICON Earth System Model

 
A team of researchers around Dr. Johann Jungclaus from the Max Planck Institute for Meteorology (MPI-M) has published a paper in the Journal of Advances in Modeling Earth Systems documenting the ICON Earth System Model Version 1.0, the first coupled ocean-atmosphere-land model based on the ICON system.  
291.

The first version of the ICON Earth System Model

 
Eyecatcher ICON- Model A team of researchers around Dr. Johann Jungclaus from the Max Planck Institute for Meteorology (MPI-M) has published a paper in the Journal of Advances in Modeling Earth Systems documenting the ICON Earth System Model Version 1.0, the first coupled ocean-atmosphere-land model based on the ICON system.  
292.

Delayed response of subsea permafrost thaw to anthropogenic warming

 
Subsea permafrost is a previously overlooked component of the climate system. In a study published in The Cryosphere, the authors Stiig Wilkenskjeld and Victor Brovkin from the Max Planck Institute for Meteorology and their former colleague Matteo Puglini together with Frederieke Miesner and Paul P. Overduin from the Alfred Wegener Institute for Polar and Oceanic Research have made a first step towards including subsea permafrost processes in an Earth System Model. The study highlights that…  
293.

Delayed response of subsea permafrost thaw to anthropogenic warming

 
Thawing rate of Arctic subsea permafrost ice for different climate projections relative to the thawing in a pre-industrial climate. Subsea permafrost is a previously overlooked component of the climate system. In a study published in The Cryosphere, the authors Stiig Wilkenskjeld and Victor Brovkin from the Max Planck Institute for Meteorology and their former colleague Matteo Puglini together with Frederieke Miesner and Paul P. Overduin from the Alfred Wegener Institute for Polar and Oceanic Research have made a first step towards including subsea permafrost processes in an Earth System Model. The study highlights that…  
294.

Marie Skłodowska-Curie Postdoctoral Fellowship for Laura Suarez-Gutierrez

 
Portrait Laura Suarez Dr. Laura Suarez-Gutierrez, scientist in the department “The Ocean in the Earth System” at the Max Planck Institute for Meteorology, successfully applied for a prestigious Marie Skłodowska-Curie Postdoctoral Fellowship. At the Swiss Federal Institute of Technology (ETH) in Zurich and the Institute Pierre-Simon Laplace (IPSL) in Paris, she will be studying the most devastating but physically plausible combinations of extreme heat. The Max Planck Institute for Meteorology warmly congratulates her…  
295.

W 2 position for Cathy Hohenegger in acknowledgement of her scientific accomplishments

 
Portrait Cathy Hohenegger Dr. Cathy Hohenegger was appointed a W 2 position in the department “The Atmosphere in the Earth System” at the Max Planck Institute for Meteorology (MPI-M). The institute warmly congratulates her on her outstanding achievements as recognized with this position. She joins Prof. Victor Brovkin and Prof. Jin-Song von Storch, both members of the department “The Ocean in the Earth System”, as one of only three scientists at MPI-M to have obtained this recognition.  
296.

New high-performance computer for Germany´s climate science

 
[Translate to English:] On March 03, 2022, the new high-performance computer system for Earth system research "Levante" started its operation at the German Climate Computing Center (DKRZ) in the first expansion stage. With 14 PetaFLOPS (14 quadrillion mathematical operations per second), the supercomputer quadruples the computing power at DKRZ.  
297.

What controls the millennial-scale climate variability in simulations of the last deglaciation?

 
[Translate to English:] The transition between the last glacial maximum (LGM, about 21,000 years before present) and present, which is referred to as the last deglaciation, was characterized by a significant warming and a series of abrupt climate changes. By conducting a first systematic ensemble of hindcast simulations for the last deglaciation with the Max Planck Institute for Meteorology Earth System Model (MPI-ESM), Marie Kapsch, Uwe Mikolajewicz, Clemens Schannwell (scientists at Max Planck Institute for…  
298.

Finding attractors of dynamical systems via recurrences

 
[Translate to English:] In a publication, recently selected as a Featured Article, in Chaos, Dr. George Datseris (Max Planck Institute for Meteorology (MPI-M)) and Associate Professor Alexandre Wagemakers (Universidad Rey Juan Carlos, Madrid, Spain) provide an algorithm that can estimate attractors and their basins for arbitrary dynamical systems.  
299.

The driving forces of the terrestrial carbon cycle predictability

 
Figure_World_map_Soil_moisture Although the global carbon cycle is predictable to some extent, we know little about the source of the memory in the system. In a study published in Earth System Dynamics, the authors Istvan Dunkl, Dr. Aaron Spring, Prof. Victor Brovkin (scientists at Max Planck Institute for Meteorology (MPI-M)) together with Prof. Pierre Friedlingstein (College of Engineering, Mathematics and Physical Sciences, University of Exeter, UK) have explored the question which environmental variables are responsible…  
300.

A Quantification of Natural Forcing Contributions on Multi-Decadal North Atlantic Temperature Variability over the Past Millennium

 
[Translate to English:] In a new study in Geophysical Research Letters Dr. Shih-Wei Fang, Dr. Claudia Timmreck, and Dr. Johann Jungclaus from the Max Planck Institute for Meteorology, Prof. Davide Zanchettin from the University of Venice and Dr. Myriam Khodri from the Institute Pierre-Simone Laplace in Paris show, that the natural external forcing, including volcanic aerosols and insolation changes, accounts for ~25% of the multi-decadal North Atlantic temperature variations in a multi-model ensemble of simulations…  
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