Project Leader and Host Organisation
Dr Richard Brinkman, Australian Institute of Marine Science
Project Description and Objectives
For detailed descriptions of the outputs for
this project for Year 4 (2009/2010) of the MTSRF Research
Programme, see the Annual Research
Plan.
An extension
task to Project 2.5i.1 is working to reveal the
underwater landscape of the northern Australian seabed by
developing a new and detailed 3D seabed map [Read more]
Hydrodynamic models simulate the advection
and mixing of water - processes fundamental in controlling the fate
and impact of freshwater, sediment, nutrients and pesticides
delivered from catchments in to the receiving waters of the Great
Barrier Reef (GBR) lagoon. We believe the modeling community is
currently in a position where it is feasible to develop a
whole-of-GBR hydrodynamic model that includes all of the important
factors affecting currents, mixing, temperature and salinity within
the GBR lagoon and exchanges with the adjacent Coral Sea.
This project aims to develop a
three-dimensional whole-of-GBR baroclinic hydrodynamic model (GBR
model) at a spatial resolution of approximately 1-2 km, with
accurate boundary forcing for offshore ocean boundaries provided by
a global, data-assimilating, eddy-resolving model. Such a
model will underpin the future development of other essential
components of a Large-Scale Water Quality (LSWQ) model, primarily
sediment dynamics and biogeochemical models, and provide a
capability to support the prediction and analysis of connectivity
and exchange of material, including larvae, throughout the GBR.
At this spatial resolution of ~1-2 km, a
critical challenge will be to deal with the range of spatial scales
encountered within the model domain, in particular the need to
resolve effects of reefs and reef passages at scales of less than
the model resolution. In order to meet this challenge, an important
part of this project will involve an investigation and assessment
of the necessity and suitability of sub-grid parameterisation
schemes within a model of this spatial resolution.
As a proof of concept for a full,
three-dimensional hydrodynamic model of the GBR, we will use the
model developed in this project to hindcast the circulation within
the GBR lagoon during the 2009 wet season, including prediction of
the trajectories and spatial distribution of major freshwater
inflows during this period.
Key objectives of this project are to:
-
Develop a three-dimensional whole-of-GBR baroclinic hydrodynamic
model, at a resolution capable of capturing the key oceanographic
processes impacting the GBR. This model is a necessary precursor to
the development of sediment dynamics and biogeochemical components
of a whole-of-GBR Water Quality Model;
-
Demonstrate proof of concept of a whole-of-GBR model through the
simulation of the circulation within the GBR lagoon during a
significant wet season, including prediction of the trajectories
and spatial distribution of major freshwater inflows during this
period; and
-
Assess the suitability of sub-grid parameterisation schemes
appropriate for application within finite difference models GBR
model.