Dr Andy Nowacki
I am a seismologist interested in global and local seismic phenomena which allow us to understand better how the Earth works, including how the interior of the Earth moves around, where and how molten material is created, and the history of our planet.
My experience includes the observation and modelling of the effects of seismic anisotropy—the variation of properties with direction—to infer deformation, encompassing mineral physics, seismic wave propagation and geodynamics. I am also interested in microseismicity in rift settings (Ethiopia and Iceland) and shallow reservoirs (geothermal and petroleum), and how earthquakes occur in the Earth's transition zone.
- Lecturer, University of Leeds (2018–)
- Leverhulme Early Career Fellow (2015–2018)
- Postdoctoral Research Assistant, University of Bristol (2012–2015)
- PhD, University of Bristol (2008–2012)
- REMIS: Reliable Earthquake Magnitudes for Induced Seismicity. In collaboration with Andrew Curtis, Brian Baptie and Corinna Roy.
I currently advise Corinna Roy on the project ‘REMIS’.
I am currently interested in supervising PhD projects in the areas of:
- Global seismic observations and modelling of mantle flow and deep mantle processes
- Automated microseismic event detection and location
- Transition zone observation and modelling
- Volcanic, geothermal and petroleum reservoir imaging, especially using seismic anisotropy
Current PhD students
- Peidong Shi – Microseismic full waveform modelling and location (with Sebastian Rost and Doug Angus, ESG Solutions)
- Jamie Ward – Seismic detection of hidden primordial regions in the Earth’s lowermost mantle (with Sebastian Rost and Mike Thorne, Utah)
- Itahisa González Álvarez – Towards an understanding of Earth's structure: the development of adaptive optics approaches for seismology (co-supervising with Sebastian Rost)
- Rebecca Smith – Mapping and characterisation of ultra-low velocity zones - Deciphering the most enigmatic deep structures of the Deep Earth (co-supervising with Sebastian Rost and Stephen Stackhouse)
- MC2: Mantle Convection Constrained
- Reliable Earthquake Magnitudes for Induced Seismicity (REMIS)
- Reliable Earthquake Magnitudes for Induced Seismicity: application to hydraulic fracturing for shale gas (REMIS)
Research groups and institutes
- Institute of Geophysics and Tectonics
- Institute of Applied Geoscience
- Deep Earth
- Geodynamics and Tectonics
- Applied Geophysics
- Planetary Exploration