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Application of Oceanographic Drift Models · Surface Drift Dynamics Tides River inflow Wind Waves...
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Application of Oceanographic Drift Models Charitha Pattiaratchi School of Civil, Environmental and Mining Engineering The UWA Oceans Institute The University of Western Australia
Transcript of Application of Oceanographic Drift Models · Surface Drift Dynamics Tides River inflow Wind Waves...
Application of Oceanographic
Drift ModelsCharitha Pattiaratchi
School of Civil, Environmental and Mining EngineeringThe UWA Oceans Institute
The University of Western Australia
Acknowledgements
Dr Sarath WijeratneDr Ivica JanekovicThe University of Western Australia
James Holder & Lucya RoncevichDepartment of Transport, WA
Pawsey Supercomputing Centre
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Tracking parcels of water
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Advecti0n
Advecti0n + Diffusion
Surface Drift Dynamics
TidesRiver inflow
Wind Waves
Stokes Drift
Environmental Forcing
Ocean Response
Drift Response
Direct Windage/
Leeway
Surface Heat Flux
Winds
Advected by near-surface
currents
Density Stratification
Depth Dependent
Currents
Vertical Mixing
Drift Modelling
Atmospheric ModelWind, temperature,
precipitation, air-sea fluxes
Particle tracking modelWater mass, debris, sediment, larvae, turtles,
wrack, oil/chemical spills, search & rescue
Ocean circulation modelCurrents, temperature, salinity,
turbulence
Wave modelStokes drift
Wave momentum
Gnomeresponse.restoration.noaa.gov
Ichthyopwww.ichthyop.org
Particle tracking model
Paul Irving, 2015
Drift Modelling: wind effects
Drift Modelling: Stokes drift
Mass transport due to waves
zu = Us
Drift Modelling: wind effects
• Surface drift due to the wind : 2 - 3% of U10
• The Ekman currents at the surface strongly depend on thevertical mixing Kz : 0.5 to 4% of U10
• Stokes drift of waves of same magnitude order : 3% of U10
Windage
Wind
Low windage, object sitting deep in water
Medium windage, object sitting half in water
High windage, object sitting high on water
Ocean surface
For example 5% windage means an object is moving with the current + 5% wind speed
Photo: Charles MoorePhoto: Randal Reeves
Photo: S/V “Tregoning”
Wind to Wind to
Wind
Direction
From
Wind
Direction
From
Wind
to
L = -25o
L = +25o
RWD = -135o
RWD = +135o
Leeway Drift
Direction
Leeway Drift
Direction
Leeway divergence
• Leeway divergence tranportobjects at an angle relative to downwind
• Symmetry allows stable drift left and right of downwind (little jibing is observed).
→Diverging search areas with time
Demo: initial conditions
Demo: advection by currents
Demo: advection by wind
Demo: advection by wind/currents
Demo: advection by wind/currents
Demo: advection by wind/currents
Demo: advection by wind/currents
Shark Bay: 2000
Particle Tracking (‘Age’)
Peddies: 3 August 2011
Peddies: Petite eddies (diameter < 25km)
Southern Surveyor Voyage
Peddie – 3 August 2010
Peddie – 3 August 2010
Temperature
ADCP currents
Northern Indian Ocean
Location & Concept Plan
Port Geographe
Sand trap
Bypass
Location & Concept Plan
Port Geographe: 24 Aug 2015
Location & Concept Plan
Port Geographe: August 2011
The Problem
The Problem
Oldham et al., 2010
Seagrass Wrack
Oldham et al., 2010
Wrack Dynamics
No detailed information available on wrack dynamics
Observations: Wrack present on beaches from May to OctoberNaturally ‘disappear’ in October/November
Hydrodynamics: Mode of transport (suspended/bedload ?)Settling velocity ?Critical shear stress ?
Stage 1 Study: Oldham C.E., Lavery P., Pattiaratchi C and Chiffings A. (2010) Research Study into Seagrass Wrack Movement in Geographe Bay
‘Summer’ - quiescent period.
Wrack accumulates offshore in meadows and adjacent un-vegetated areas.
‘Winter’ - storm period.
Wrack is moved into surf-zone & beach. Whilst in the surf-zone, subject to long-shore transport.
Wrack ‘life-cycle’
Late Winter/Spring.
Wrack is removed from naturally from the beaches.
Particle conceptual model
Resuspension
v
c
Transport (Currents, Stokes drift, Diffusion)Deposition (when zp<=zo)
Beach accumulation (τc increase and ws=0)
Resuspension from the beach (ws decrease back to initial)
Bathymetry: existing/proposed
Wrack transport
Post construction
Construction completed in June 2014: ~ $27 million
Search for MH370
Disappeared on 8 March 2014
Area 1
Area 2
Area 3
MH370: initial search areas
Search for MH370
Predictions: August 2014
Predictions: August 2014
MH370: simulations
Pawsey Supercomputing Centre
MH370: simulations
MH370: simulations
MH370: simulations
Thank you
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