Predicting and Validating Ocean Response to Severe Tropical Cyclones at North West Shelf of WA

Within this project we are investigating ocean-atmosphere interactions using the latest modelling tools at high spatial and temporal resolutions. The key element that is currently missing in the ocean (and atmosphere) modelling predictions is lack of exchange of information between ocean and atmosphere. To resolve that issue we are using 3 models (ocean, wave and atmosphere) 2-way coupled (each model can receive and send information) at 10 minute interval. Example of that interaction is ocean-atmo dynamics that took place during TC Veronica at WA.
Person

Principal investigator

Ivica Janekovic ivica.janekovic@uwa.edu.au
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Area of science

Physical Oceanography
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Systems used

Magnus
Computer

Applications used

Numerical models for ocean and atmosphere
Partner Institution: The University of Western Australia| Project Code: 2070

The Challenge

What is the effect of non-coupling (classical and usual approach) versus fully 2-way coupled system? What are gains if we include better formulations for ocean surface (such as better surface wind drag, cooling, heat flux) influencing at the same time ocean and atmosphere (lower boundary condition)? Is it important for tropical cyclone dynamics to include correct feedback from the ocean?

The Solution

Using timely 2-way exchange of information between all models used to simulate ocean or/and atmosphere dynamics we should get better solution for all of them. This is relevant topic for analysing ocean (and atmosphere) processes during the severe tropical cyclones occurring at the North West shelf of WA.

The Outcome

Using Pawsey supercomputer infrastructure we are able to simulate complex dynamics in the ocean and atmosphere and more importantly interactions between them that are intimately linked. Solution of that system is superior when compared to classical approach when there is no such information exchange. Fast interconnections and big number of cores provide perfect framework for such problems.

 

 

Significant wave height during TV Veronica
Surface ocean currents during TC Veronica