217.

Observations

 
Observations are data records collected with the help of scientific measuring instruments. There are, for example, countless weather stations around the world that measure temperature on land, in the air and in the sea as well as satellites, ships and aircraft that also take measurements of various variables. Observations are enjoying a renaissance at the Max Planck Institute for Meteorology. There are two main reasons for this. One is that the main tools we use to study the climate…  
218.

The effect of climate perturbations on the timing of Heinrich events

 
[Translate to English:] Throughout the last glacial period (ca. 65,000-15,000 years before present) periodic ice discharge events from the North American ice sheet, known as Heinrich events, shaped the climate evolution of the northern Hemisphere. However, the driving mechanisms behind these events remain elusive to this day. In a new study, Schannwell et al. investigate the sensitivity of Heinrich events to different climate perturbations. They find that changes in snowfall and surface temperature can pace the timing…  
219.

AMOC sensitivity to icebergs

 
AMOC sensitivity to iceberg forcings The last glacial cycle was characterized by a number of abrupt cooling events in the North Atlantic known as Heinrich events. Heinrich events are associated with massive ice sheet surges from the former Laurentide ice sheet and subsequent predominantly eastward transport of icebergs across the North Atlantic. Paleo records also indicate that ice discharge events coincided with a weakening of the Atlantic Meridional Overturning Circulation (AMOC). Typically,…  
220.

Self-sustained AMOC oscillations

 
AMOC response to different forcing and self-sustained AMOC oscillations State-of-the-art coupled climate models produce very different states of the Atlantic Meridional Overturning Circulation (AMOC) in simulations of the Last Glacial Maximum (LGM). Many of them fail to capture the shoaling of the North Atlantic Deep Water (NADW) cell, as indicated by paleo records. The mechanisms that control the shoaling are not yet well understood. Changes in the AMOC have also been linked to past abrupt…  
221.

Fully coupled climate-ice sheet simulations

 
Fully coupled climate-ice sheet simulations of the last deglaciation The climate system has undergone dramatic changes during the last deglaciation from 21,000 years before present to present day. For example, the Laurentide ice sheet over North America and the Fennoscandian ice sheet over Northern Europe have completely disappeared. This collapse of the ice sheets was accompanied by a global sea-level rise of ~120 m. The individual climate components and their responses to changing conditions…  
222.

nextGEMS

 
Duration 09/2021–08/2025 Duration Funded by nextGEMS is funded through the European Union’s Horizon 2020 research and innovation program under the grant agreement number 101003470. Funded by Lead Principal Investigators Bjorn Stevens (MPI-M), Irina Sandu (ECMWF) Lead Principal Investigators Contact Dr. Heike Konow Dr. Theresa Mieslinger Dr. Elina Plesca nextgems_office@mpimet.mpg.de Contact nextGEMS: Next Generation Earth Modelling Systems nextGEMS (next Generation Earth…  
223.

Extreme Storm Floods

 
Past and Future Variability of Extreme Storm Floods in the southern North Sea The low-lying coasts of the southern North Sea are particularly exposed to extreme sea levels (ESL) in form of storm floods. Due to anthropogenic climate change, the risk of flooding is expected to increase in the future (IPCC, 2019). Adequate and timely coastal protection relies on estimates of expected heights and frequencies of such ESL events, particularly of the policy-relevant high-impact-low-probability…  
224.

Is climate deterministic or stochastic?

 
Prof. Jin-Song von Storch shows in a new paper that climate variability on ultra-long timescales is, contrary to common understanding, not determined by the responsible internal dynamics on the same timescales. Her study is an impetus for a new way of thinking. Her result provides first evidence showing that climate as a dynamical system is not deterministic in an absolute sense.  
225.

Application

 
This is what you bring: A first class Master’s degree with written thesis (!) in physics, geophysical sciences (incl. meteorology and oceanography), ecology, mathematics, computer science, engineering, economics, or political science Students currently working on their MSc thesis are also encouraged to apply The study and work load for both your degrees (MSc and BSc) amount to (at least) 300 ECTS (or an equivalent to this) This is what you bring: Dates (of a general annual call) …  
226.

Structure and Support

 
Prof. Dr. Sarah M. Kang Head of IMPRS-ESM Tel.: +49 (0)40 41173-437 sarah.kang@mpimet.mpg.de Name;First name;Email;Institute;Executive Committee Ament;Felix;felix.ament@uni-hamburg.de;UHH; Bader;Jürgen;juergen.bader@mpimet.mpg.de;MPI-M; Baehr;Johanna;johanna.baehr@uni-hamburg.de;UHH, IfM;Executive Committee Bao;Jiawei;;ISTA, Austria; Bieser;Johannes;Johannes.Bieser@hereon.de;Hereon; Bister;Marja;marja.bister@helsinki.fi;University of…  
227.

People and Academic Environment

 
Name Research Group Email Alastrue de Asenjo, Eduardo Climate Modeling Group eduardo.alastrue-de-asenjo@mpimet.mpg.de Andernach, Malena Ocean Physics malena.andernach@mpimet.mpg.de Antary, Nils Clouds and Convection nils.antary@mpimet.mpg.de Bayley, Clara Drivers of Tropical Circulation clara.bayley@mpimet.mpg.de Behncke, Jacqueline Observations, Analysis and Synthesis jacqueline.behncke@mpimet.mpg.de Boza, Evangelina Institute of Oceanography evangelia.bosza@mpimet.mpg.de Breunig,…  
228.

Training

 
The IMPRS-ESM curriculum is flexible. In addition to a few basic training units it also allows to accommodate training interests voiced by doctoral candidates! These two principal teaching units are offered annually: Introduction to Earth system sciences and modelling (1st year mandatory course) Annual Retreat (mandatory event) Please note: A large number of IMPRS-ESM courses are offered according to demand from participants and the scientific expertise of the lecturers. You as…  
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