Julius Eberhard- Master of Science
- Doctoral Researcher at Potsdam Institute for Climate Impact Research
Julius Eberhard
- Master of Science
- Doctoral Researcher at Potsdam Institute for Climate Impact Research
Investigating the role of climate in the evolution of plate tectonics, esp. during and after extensive glaciations
About
5
Publications
512
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16
Citations
Introduction
My research centers around modeling the climate and adjacent domains of the Earth system. Currently, I investigate the interaction of climate and plate tectonics via surface processes. Previously, I worked on the effects of orbital variations and volcanic perturbations on a “Snowball Earth” inception, current Arctic atmospheric dynamics, and current and future surface processes of the hydrosphere. I got education in physics and geoecology and developed particular interest in nonlinear phenomena.
Skills and Expertise
Current institution
Additional affiliations
November 2014 - August 2015
Position
- Bachelor's Student
Description
- Modeling of coastal salinization (bachelor thesis). Model: SWAP. Referees: Dr. N.L.M.B. van Schaik, Dr. Thomas Graeff. Great support from N.L.M.B. van Schaik, Thomas Graeff, and Anett Schibalski.
April 2018 - September 2018
Position
- Bachelor’s Student
Description
- Statistical analysis of internal variability of a coupled Arctic regional climate model (bachelor thesis). Model: HIRHAM–NAOSIM. Referees: Dr. Annette Rinke, Prof. Markus Rex. Possible with a lot of help and care from Annette Rinke, Yu Xiaoyong, Wolfgang D., and Sabine E.
September 2020 - March 2022
Position
- Master's Student
Description
- Perturbation experiments on a global glaciation (“Snowball Earth”) during the Neoproterozoic (master thesis). Model: CLIMBER-3α. Referees: PD Georg Feulner, Prof. Arkady Pikovsky. Fantastic support from Georg Feulner, Stefan P., Mona Bukenberger, and Jan Landwehrs.
Education
October 2018 - March 2022
April 2016 - September 2018
October 2012 - March 2016
Publications
Publications (5)
The Cryogenian period (720–635 million years ago) in the Neoproterozoic era featured two phases of global or near-global ice cover termed “snowball Earth”. Climate models of all kinds indicate that the inception of these phases must have occurred in the course of a self-amplifying ice–albedo feedback that forced the climate from a partially ice-cov...
The Cryogenian period (720–635 million years ago) in the Neoproterozoic era featured two phases of global or near-global ice cover, termed ‘Snowball Earth’. Climate models of all kinds indicate that the inception of these phases must have occurred in the course of a self-amplifying ice–albedo feedback that forced the climate from a partially ice-co...
Salinization is a well‐known problem in agricultural areas worldwide. In the last 20–30 yr, rising salinity in the upper, unconfined aquifer has been observed in the Freepsumer Meer, a grassland near the German North Sea coast. For investigating long‐term development of salinity and water balance during 1961–2099, the one‐dimensional Soil–Water–Atm...
Predicting the 2018 Heatwave and Fires in Sweden
Salinization is a well-known problem in agricultural areas worldwide. For the last 20–30 years, rising salinity in the upper, unconfined aquifer has been observed in the Freepsumer Meer, a deep grassland area near the German North Sea coast. In order to investigate long-term development of soil salinity and water balance, the one-dimensional SWAP m...
