Full description
The dynamics of the seasonal evolution of chlorophyll a at the continental shelf break around 32 degrees south has been investigated using a one-dimensional numerical BGC model at shelf and lagoon scales. The results show that a combination of vertical mixing associated with the Leeuwin Current and surface cooling during the winter months is responsible for the wintertime increase in chlorophyll a concentration at the shelf break (Greenwood and Soetaert, 2008). In addition, variation in the timing and magnitude of the winter increase in chlorophyll is shown, for the first time, to relate to the strength of the Leeuwin Current. A nitrogen budget for the southwest WA shelf has been derived by diagnosing the simulated fluxes of particulate and dissolved nitrogen from the 3-D model across the shelf boundaries (across two cross-shelf transects at 27S and 34.5S and across the 100 m isobath) as well as deposition and release of nitrogen at the seafloor.Lineage
Progress Code: completed
Maintenance and Update Frequency: notPlanned
Statement: A coupled three-dimensional hydrodynamic-biogeochemical model (ROMS) has been configured for the southwest shelf off Western Australia. The primary task of the model is to simulate seasonal changes in phytoplankton chlorophyll concentrations and help quantify seasonal fluxes of nitrogen on and off the shelf. The model domain extends from the coast to offshore 108oE and from 35oS (Cape Leeuwin) to 21oS (the North West Cape). The horizontal resolution in cross-shore direction varies between 2 km and 4 km from the coast to the 1000 m isobath and then increases to 8 km at the oceanic boundary. The alongshore resolution varies from 3 km to 8 km. There are 30 vertical levels with refinement in the top 200 m. Full details of the hydrodynamic model are given in chapter 1. The biogeochemical model describes pelagic and benthic aspects of nitrogen cycling.The pelagic model is NPZD in nature, and includes seven state variables: phytoplankton (PHY), zooplankton (ZOO), nitrate (NO3), ammonium (NH4), small and large detritus (SDET and LDET), and phytoplankton chlorophyll (CHL).
Notes
CreditJim Greenwood
Credit
Liejun Zhong
Liejun Zhong
Credit
Peter Craig
Peter Craig
Credit
Ming Feng and Karen Wild-Allen
Ming Feng and Karen Wild-Allen
text: westlimit=20; southlimit=-70; eastlimit=127; northlimit=28
Subjects
Coastal Waters (Australia) | West Australia Coast West, WA |
Global / Oceans | East Indian Ocean |
Global / Oceans | Indian Ocean |
WAMSI Node 1 Project 1: Southwest Australian Coastal Biogeochemistry |
Western Australian Marine Science Institute |
oceans |
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Other Information
Identifiers
- Local : Anzlic Identifier: ANZCW0306008584
- Local : Marlin Record Number: 8584
- global : 8002c12d-f599-4dde-878b-8d7fc39fd992
