Research for the Ocean State
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Scientists deploying instruments
from the national research ship, Southern Surveyor, during
the research voyage off the Western Australian coastline.
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Released: 18 February 2004 (by CSIRO Marine and Atmospheric Research)
With 40% of Australias coastline, and some of the most
economically important marine developments in the country, it
is important for WA to have the information needed to manage
and develop marine resources responsibly.
The Leeuwin current is one of the major marine influences in
Western Australia.
The influences of the Leeuwin Current, on Western Australias
unique marine ecosystems, have come under the spotlight in a
series of successful research voyages by State and National
research agencies.
"There is no other ocean current in the world like the Leeuwin.
It transports warm, unproductive water off the west coast of
a continent. The Leeuwin flows in the opposite direction to
similar currents off other continents," says CSIRO ecologist
Dr Tony Koslow.
"We are at the very beginning of understanding how it influences
the food webs that support the lobster, salmon and pilchard
fisheries, among many others, and how it supports the wealth
of ocean life and rich economic return enjoyed off Western Australia."

One element of a set of instruments
enabling scientists to study daytime and night time cycles
in which some species rises hundreds of metres at night
to feed. |
Dr Koslow was Chief Investigator on the most recent research
voyage on the national research ship, Southern Surveyor,
which returned to Fremantle this week after eight days at sea.
The voyage is one of four by Southern Surveyor to
study the south west Australian marine ecosystem conducted under
the Strategic Research Fund for the Marine Environment (SRFME).
SRFME is a six-year, $20 million partnership between the West
Australian Government and CSIRO in collaboration with West Australian
universities.
Dr Koslow said the work, sampling the ocean from shallow waters
just a few kilometres off the coast north of Perth, across the
continental shelf and out to depths of 1,000 metres over the
continental slope, will provide a baseline against which future
changes in the marine ecosystem can be measured.
On board the 65-metre Southern Surveyor, scientists
worked around-the-clock deploying an armoury of nets and other
sampling instruments that enabled them to study daytime and
night time cycles as well, in which some species rise hundreds
of metres at night to feed.
Click here
to watch a net being deployed (Quicktime
movie file 2.6MB)
"The focus of our cruise is on understanding how the pelagic
or midwater ecosystem varies from nearshore to offshore: differences
in the food webs, their seasonal cycles and how climate cycles
like El Nino affects it as well.
"Theres a naturally-occurring balance in the waters
off Western Australia that is governed by the Leeuwin, and how
strongly its flowing, which is influenced in turn by climatic
factors in other oceans such as El Nino.
"Through measuring and observing ocean life, and combining
this with satellite observations of the Leeuwin and local currents
and eddies we can better understand the factors integral to
sustaining the ocean food web.
"The long-term goal of our study is to build a predictive capability
for fisheries and coastal resource managers related to climate
change in the ocean," Dr Koslow said.
Australian science is building an ocean forecasting capacity
through the research project, BlueLink (http://www.marine.csiro.au/bluelink/)
With the marine environment being a significant contributor
to the States economy the current scientific research
will add to the knowledge base being generated through the collaborative
SRFME research program.
Dr Koslow said a key feature of the research partnership of
this and related SRFME projects is the advanced education program
training marine scientists.
Scientists and technicians from CSIRO, and University of Western
Australia, Curtin, and Murdoch participated in the voyage.
For further information please contact:
Dr Tony Koslow 08 9333 6520
Mr Don Michel 0419 314 434
Background
What is SRFME?
The Strategic Research Fund for the Marine Environment (SRFME)
is a $20 million, six year joint venture between CSIRO and the
Western Australian Government. The research fund aims to enhance
the capability and capacity of marine science in areas of strategic
interest to the WA government.
SRFME will invest in a number of large integrated marine science
projects to be conducted by CSIRO, in collaboration with state
and federal agencies, and in PhD scholarship projects. Importantly
the research funded by SRFME will be strategic as opposed to
applied or tactical research aimed at a particular single industry
or management objective (which is more appropriately funded
by other sources). It will therefore serve the long-term needs
of Western Australia across a range of user groups from fisheries
to ecosystem management.
The State Government Agencies involved in SRFME are: the Department
of the Premier and Cabinet; Department of Conservation and Land
Management; Department of Fisheries WA; Department of Environment,
Water & Catchment Protection and the Department of Industry
and Resources. For more information on SRFME, please contact
the Research Director, Dr John Keesing on (08) 9222 8887 at
Office of Science and Innovation, Depart. of the Premier &
Cabinet, Level 2, 197 St George's Terrace Perth WA 6000.
About the Project
Western Australia is arguably the region most sensitive to
climate variability in Australia. The strength of the Leeuwin
Current and Indonesian throughflow, and major
regional fisheries (e.g. western rock lobster, pilchard and
scallops) all respond strongly to the El Nino-Southern
Oscillation cycle. However, present understanding is rudimentary
of the regions biological oceanography, the presumed link
between ocean forcing and the fisheries. The seasonal cycles
of biological productivity on the continental shelf and slope,
and the spatial distribution of production regimes still remain
largely unknown. Much less is known about interannual variability
and the factors driving such variation.
Management of marine resources and habitats requires that scientists
distinguish the effects of natural climate variability and climate
change from anthropogenic effects. The aim of the project is
to examine how climate forcing influences nutrient, phytoplankton,
zooplankton and micronekton dynamics across the shelf with application
to fisheries, management of marine protected areas and coastal
processes.
This project is closely linked with the modelling and coastal
projects. It is strategic and will provide a quantitative understanding
of biophysical dynamics across the continental shelf. During
the second half of the project, proposals will be made in collaboration
with WA partners to apply our emerging understanding to specific
issues in fisheries and/or the management of MPAs and the coastal
zone.
More about Project 2: The
biophysical oceanography off Western Australia
About the Leeuwin Current
Australia is influenced by four major ocean currents
- The Leeuwin Current
- The East Australian Current southward flowing
from near Fraser Island to Tasmania
- The Indonesian Throughflow a system of westward
flowing currents from the Pacific to the Indian Ocean
- The Antarctic Circumpolar Current the worlds
largest ocean current and considered the powerhouse for global
climate.
The Leeuwin Current takes an opposite course to geographically-similar
currents which flow northward up the African (Benguela) and
South American (Humboldt) continents.
Partly formed from the system of currents draining the Pacific
Ocean into the Indian Ocean through Indonesia, its characteristics
are detectable throughout the course of its long winter journey.
The journey is governed by seasonal conditions and prevailing
winds, with the Current generally following the edge of the
continental shelf.
The southward flow of the Leeuwin is weakest from
November to March when the winds tend to blow strongly northwards
and reaches greatest flow is in the autumn and winter when the
opposing winds are weakest.
In the Indian Ocean, typical current speeds in the Leeuwin
Current and its eddies measured are about 1 knot although
speeds of 2 knots are common, and the highest speed ever recorded
by a drifting satellite-tracked buoy was 3.5 knots. The Leeuwin
Current is about 300 m deep (quite shallow for a major
current system, by global standards), and beneath it is a northwards
countercurrent called the Leeuwin Undercurrent.
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