Dr. Paul Eizenhöfer

Professor

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Biography

Dr. Paul Eizenhöfer is a Senior Lecturer in the School of Geographical and Earth Sciences at the University of Glasgow. He has extensive experience in Computational Geoscience and has held various academic positions since 2018, including Assistant Professor and Postdoctoral Fellow roles at notable institutions such as the University of Tübingen and the University of Pittsburgh. His research interests focus on the interplay between tectonics, climatic drivers, and landscape evolution, employing multidisciplinary approaches that integrate empirical and computational methods. Dr. Eizenhöfer is particularly interested in using UAV and satellite-based remote sensing for geomorphological analysis and the reconstruction of Earth's crustal evolution. Additionally, he is committed to developing locally tailored strategies to protect natural and anthropogenic ecosystems in response to climate change. Eizenhöfer has received substantial funding for his research projects, reflecting his active engagement in the scientific community. He also contributes to academia through various editorial roles and peer reviews for more than 30 international journals.

Research Interests

Experience

Senior Lecturer / Associate Professor

2024-01-01 — Present

University of Glasgow • Glasgow, Scotland

Teaching and research in the field of Computational Geoscience.

Lecturer / Assistant Professor

2022-01-01 — 2024-01-01

University of Glasgow • Glasgow, Scotland

Engaged in teaching and mentoring in the School of Geographical and Earth Sciences.

Wissenschaftlicher Mitarbeiter (Post-Doc)

2018-01-01 — 2022-01-01

Universität Tübingen • Tübingen, Germany

Research focused on Cenozoic evolution in the Alps.

Humboldt Postdoctoral Fellow

2015-01-01 — 2018-01-01

University of Pittsburgh • Pittsburgh, USA

Conducted research on the evolution of the eastern Himalayan fold-thrust belt.

Research Assistant

2014-01-01 — 2015-01-01

University of Hong Kong • Hong Kong, China

Contributed to research on the Permian/Triassic closure of the Palaeo-Asian Ocean.