Junior Research Groups
The junior research groups at the Alfred Wegener Institute are funded by the Federal Ministry of Education and Research, the Helmholtz Association and the European Research Council. There are currently 11 such groups at the institute.
Current call for applications for Helmholtz Junior Research Groups
The 15th call for Helmholtz Junior Research Groups was published on 17 January 2018. The documents are available online here:
The deadline for applying a Helmholtz Young Investigators Group at AWI is March 01, 2018. Curriculum vitae, list of publications and 2 pages of project summary should be sent to email@example.com. The internal selection of project takes place together with the AWI Scientific Council and based on the following criterions:
Scientific excellence – The proposed project should meet the criterion of science excellence as indicated by colleagues in the Scientific Council, independent of the particular research theme or focus.
2. Candidate´s Excellence – the candidate should demonstrate in their Curriculum Vitae true excellence in training and experience, including early independence, supporting the project in 1., above
3. Compatibility with AWI´s Program Oriented Funding (POF) – The project should, as far as possible, integrate with and build on the ongoing research being planned at the AWI. If the work is in an entirely new research area, this should be discussed and justified specifically
4. Connection with a German university
Deadline for nomination by AWI is May 04, 2018.
Helmholtz Junior Research Groups
With the Helmholtz Junior Research Groups, the Helmholtz Association supports the early independence of young scientists and offers them a reliable career perspective. This programme is designed to provide outstanding working conditions in a research-oriented environment for the best foreign and domestic junior researchers. It is aimed at junior employees who have completed their doctorates within the past two to six years.
Further information about this programme can be found on the pages of the Helmholtz Association
BMBF FONA Programme
Within the framework of the BMBF-FONA-Programme (Research for Sustainable Development), decision bases for future-oriented action will be developed and innovative solutions for a sustainable society will be delivered. With the third framework programme (FONA³), this sustainability research in Germany is supported by the Federal Ministry of Education and Research. The funding programme "Junior Research Groups on Global Change - 4+1" enables young scientists to meet the challenges of global change with exceptional and innovative research ideas and to find feasible solutions.
For further information, please visit the website of the Federal Ministry of Education and Research (BMBF)
ERC Starting Grant Junior Research Groups
ERC Starting Grants support aspiring research group leaders who want to establish a well-equipped research team and conduct independent research in Europe. The programme is aimed at promising researchers with proven potential to become independent leaders of a new and excellent research team. It is aimed at junior employees who have completed their doctorates within the past two to seven years.
For more information, visit the European Research Council website.
The decline in sea ice is one of the most prominent features of climate change. In addition to the ecological and socio-economic effects of ice loss, the associated changes in the global climate system are becoming increasingly important. Sea ice is not only sensitive to climate change, it also influences it. The aim of the Helmholtz Junior Research Group PALICE is to investigate the interactions between changes in sea ice cover and oceanic and atmospheric circulation during past climate fluctuations.
The research focus of the EcoTrace Group is to gain a better understanding of the role of trace metals in the ecology of Antarctic microalgae and to clarify the effects of global climate change on microalgae in the Southern Ocean.
The research focus of the SEAPUMP group is on understanding the role of the ocean and the biological pump in the global carbon cycle. In order to assess the current and future absorption of carbon dioxide by the biological pump, a quantitative understanding of the structure and function of marine food webs and their interaction with export processes is necessary. This is the only way to predict changes in carbon exports.
The effect of deformation mechanisms for ice sheet dynamics
The large ice masses, stored in the polar ice sheets, are the Earth's main freshwater reservoirs and therefore have a potentially enormous effect on the development of sea level. In particular, the role and development of ice flows such as NEGIS are still highly controversial. IPCC showed that the ice flow dynamics and thus the physical processes of ice movement towards the ocean and estimations are insufficiently understood. The ice flow dynamics must therefore be seen as the main source of error for sea level predictions. We study one of two main components controlling the dynamic flow: the internal deformation of the ice body.
PermaRisk deals with the simulation of erosion processes in permafrost landscapes against the background of climate change and includes a risk assessment for ecosystems and infrastructure in the Arctic.
PlanktoSERV assesses the effects of simultaneous changes in temperature, pH, nutrients and salinity on plankton communities, thus contributing to a reliable understanding of future changes in ecosystem services.
The overarching goal of SSIP (Seamless Sea Ice Prediction) is to advance sea-ice prediction capacity on timescales from hours to years and beyond. Numerous research avenues will be taken towards this goal, along the way how we observe the sea ice as well as the atmosphere and the ocean, how we feed these observations into our forecast models in a process called data assimilation, and how our models simulate the physics that determine how the sea ice ecolves in the future.
In the PETA-CARB project we are investigating the size, quality and dynamics of carbon repositories in Arctic permafrost soils and deep sediments and combine this with remote sensing studies to make quantitative statements about the landscape dynamics of fast permafrost thawing and its influence on the global carbon cycle.
SPACE (Space-time structure of climate change) determines the spatial and temporal structure of climate change on time scales from years to millennia. This structure allows us to test climate models, improve our understanding of climate variability and provide a more solid basis for climate reconstruction.