Senior Research Scientist – Sea Level
National Oceanography Centre – Liverpool
Introduction
I'm a computational ocean (data) scientist who generally develops methods to make the most of the imperfect numerical models/theories and the sparse/aliased observations we have of the ocean. My application focus has included understanding ocean/climate dynamics and improving existing or exploring alternative observational methods to monitor basic ocean state variables. I have approached these applications by developing/running experiments with ocean/climate models, estimating data products for assimilation by forecasting systems, probing how existing/hypothetical data could be used in ocean state estimation, and investigating how to enhance ocean observing systems. I generally choose my research topics by thinking of an application that allows me to both learn something new about the earth system and add a new computational/statistical method to my tool-belt. In my spare time, I compose and release music, sometimes for outreach but most of the time just as an outlet.
Research
Summary:
Computational physical oceanography (using models to identify how to improve ocean state estimates as well as parameterize and understand interactions at oceanic boundaries)
Ocean data science (combining information from theories, numerical/empirical models, and observations to estimate environmental conditions as well as assess and design observing systems)
The primary research questions I focus on include:
What are the roles of the ocean circulation and mixing in determining ocean and climate variability and change?
How can we best reconstruct and understand ocean properties of the recent past using a combination of available observations and models?
How can we improve future forecasts through the assimilation of existing or hypothetical observational platforms and/or development of physically-motivated model parameterizations?
A few example findings from my research include:
Form drag-induced dissipation dominates lee wave drag-induced dissipation in the ocean and can enhance near-bottom velocities via topographic deflection
Ocean circulation changes with increasing carbon dioxide buffer both surface temperature changes and ocean deoxygenation
Variables you can invert from magnetic field data can help monitor ocean heat content and ocean circulation variability
See my publications for more detail
Education