About
I'm a planetary scientist at the University of Münster, curious about how planets and moons work from the inside out. My research looks at the interiors of icy moons — from the thermo-chemical evolution of their metallic cores to convection in their ice shells — and, more recently, at the surfaces of small bodies like asteroids and comets. I love exploring how different processes connect, how similar patterns appear across worlds, and how theory and observation can come together to tell a more complete story.
My fascination with space started early. In 9th grade, I did a school internship at the Institute for Planetary Research at the German Aerospace Center in Berlin. After studying physics at Humboldt University of Berlin, I found myself back at the same institute for my PhD work and earned my doctorate from the University of Münster in 2018. I'm now a postdoctoral researcher in Bastian Gundlach's experimental planetology group at Münster.
Outside of research, I'm usually orbiting a different kind of chaos — life with three kids, a curious mind, and my partner in crime. We love spending time outdoors, building things, or diving into creative projects together. It's a full, sometimes hectic, but always inspiring universe.
Research Projects
Planetary Core Dynamics & Magnetism
Core solidification, dynamo processes, magnetic field generation, Fe–FeS systems.
Icy Ocean Worlds
Ice shell convection, coupling between ice and mushy layers at the ice–ocean interface, material exchange.
Small Body Surfaces
Subsurface thermo-physical evolution, sintering processes, volatile transport.
Current Positions
Scientific Staff Member (Wissenschaftliche Mitarbeiterin)
Publications
Icy ocean worlds - astrobiology research in Germany
Terrestrial planet surfaces and interiors
The Origin of Ganymede's Internal Magnetic Field
Lunar Magnetism
Large Ocean Worlds with High-Pressure Ices
Ice-Ocean Exchange Processes in the Jovian and Saturnian Satellites
Experimental and simulation efforts in the astrobiological exploration of exooceans
Top-down freezing in a Fe-FeS core and Ganymede's present-day magnetic field
Iron snow, crystal floats, and inner-core growth: modes of core solidification and implications for dynamos in terrestrial planets and moons
The Fe snow regime in Ganymede's core: A deep-seated dynamo below a stable snow zone
A long-lived lunar dynamo powered by core crystallization
Physical state of the deep interior of the CoRoT-7b exoplanet
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