Post-Doc: Data integration, model interfaces and knowledge transfer
Project leader
Yi-Wei Chen
Advisors (int.)
Prof. Roland Pail, Prof. Hans-Peter Bunge, Prof. Michael Krautblatter
Advisors (ext.)
Prof. Dr. van der Meijde (Univ. Twente)
Description
A key aspect in the proposed RTG is to find a common language between all involved scientific fields, i.e. geodesy, geology, geophysics, mathematics and informatics. In particular, the integrated process model (PC IV) requires the integration of data from various fields into one synthetic model and building the bridge between the different components of the integrative model. Here, essential elements will be data acquisition, data preparation, and first analyses and modelling attempts under the view of the joint UPLIFT research objective.
Moreover, as a second key aspect, since this post-doctoral project combines and unites the results of most of the doctoral projects, it will support significantly the knowledge transfer between doctoral cohorts I and II.
For the Post-Doc, the integrative objective of this project at the interface of the disciplines, but also at the core of the central physical process model, will significantly contribute to his/her further qualification and shaping the personal profile, because the acquired competencies are pre-requisites for a future leading role, such as a professorship or a position in science management. The Post-Doc shall work on his/her habilitation during the RTG period.
Motivation
Vertical motions of the Earth’s lithosphere away from an isostatically compensated state provide a powerful lens into the dynamic behavior of the sublithospheric mantle. The combination of geodetic and geologic observations provides extraordinary opportunities to constrain deep earth processes in geodynamic forward and inverse models of past mantle convection.
Main objectives
- Integrating geodynamical, geological, geomorphological and geodetic data into a synthetic model.
- Systematic up- and downscaling of respective datasets and physical parameters.
- Development of model interfaces to connect the geodynamical model to the geomorphological model and the geodetic model (geodynamic gross uplift – geomorphological rock weathering = geodetic net uplift)
- Knowledge transfer from cohort I to cohort II
RTG coupling
- An integrative view over all doctoral projects P1 – P10
- A close link to the second integrative project P9, uncertainty distribution among all data and model components
Preliminary results
I have compiled datasets from different Uplift projects (and from literature). Currently, I focus on a regional-scale compilation in North America. By compiling stratigraphy records, airborne magnetic data, magmatic geochemistry, and geodynamic modeling results, I mapped the spatial extent of the 20-Myr unconformity in the western US, interpreted here as the surface uplift due to the Yellowstone plume impingement in the early Miocene.
Presentations and publications
Chen, Y.-W. and Wu, J.: Lesser Antilles slab reconstruction suggests significant northwestwards lateral slab transportation underneath the Caribbean, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-1352
Chen, Y.-W., Bunge, H.-P., Stotz, I., and Wu, J.: Testing tomography-based plate reconstructions from a paired, inverse-forward closed-loop experiment in a mantle circulation model, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3083
Chen YW, Wu J, Goes S. 2024 Lesser Antilles slab reconstruction reveals lateral slabtransport under the Caribbean since 50 Ma. Earth and Planetary Science Letters 627, 118561.
Chen YW, Wu J, Bunge HP, Stotz I, Robl G, Schuberth BSA (submitted) Tomopac2: an unfolded-slab plate reconstruction validated via mantle circulation models in a closed-loop experiment. Proceedings of the Royal Society A: Mathematical Physical and Engineering Sciences