Waves, Wakes and Water Clarity - lwli.org WEMo • BoMo - forecast boat wake waves, sediment motion...

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10 January 2016 Waves, Wakes and Water Clarity: Understanding Physical Drivers of Seagrass Distribution in Coastal Waters Mark Fonseca, Ph.D. CSA Ocean Sciences Inc. Amit Malhotra, MSc., GISP Geohorizons

Transcript of Waves, Wakes and Water Clarity - lwli.org WEMo • BoMo - forecast boat wake waves, sediment motion...

Page 1: Waves, Wakes and Water Clarity - lwli.org WEMo • BoMo - forecast boat wake waves, sediment motion • OWMo –forecast light availability using bathymetry and ... Waves, Wakes and

10 January 2016

Waves, Wakes and Water Clarity: Understanding Physical Drivers of Seagrass Distribution in Coastal Waters

Mark Fonseca, Ph.D.CSA Ocean Sciences Inc.

Amit Malhotra, MSc., GISPGeohorizons

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Problems and Solutions – Physical Drivers of Seagrass Landscape Dynamics

Likely Physical Drivers

• Wind Waves

• Vessel Wakes

• Spatial and Temporal Light Availability

Tools Highlights

• WEMo – Wave exposure model (+ higher order tools)

• BoMo – Boat wake model (method)

• OWMo – Optical water quality model (method)

Opportunities and Issues

• Applications

• Average Conditions versus Extreme Events

• Traction

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Wind waves and currents influence seagrass landscapes across hydrodynamic gradients

3More Patchiness + More Frequent Spatial Change

Increasing Tidal Currents and/or Wave Energy

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Recomputed from Fonseca and Bell, 1998

Tipping point? Wind waves and cover

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CSA Dcaan Sciancaa Inc.

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Wave forecasting tools

• SWAN – Complex model to compute waves generated by wind and swells– Wave propagation; refraction, diffraction and dissipation (shoaling, whitecapping, bottom

friction, vegetation, breaking and turbulent flow)– Complex and time consuming computations– Well reviewed by scientific community

• DELFT3D – 3D model which includes SWAN along with modules for sediment transport and water

quality– Complex and time consuming computations– Well reviewed by scientific community

• WEMo – wave modeling for ecologists

– Simplified model to compute local wind waves - not swells– Wave propagation and dissipation (shoaling, white capping, bottom friction and breaking)– Module for forecasting sediment initiation of motion– Does not explicitly compute refraction / diffraction – Easier to run and less computationally intensive– Verified– Few publications

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Application

• We have tools

• We have theory

• Can we apply this concept to mitigation?

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Application: NC Bonner Bridge Mitigation

Reduce wave energy on patchy seagrass beds

Facilitate bed coalescence

Increase cover per unit area seafloor

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WEMo wave reduction + seagrass response

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CSA Dcaan Sciancaa Inc.

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Wave break installation – NC (Jan. 2017)

CSA Dcaan Sciancaa Inc.

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Vessel Wakes – Marine Corps Base Camp Lejeune

CSA Dcaan Sciancaa Inc.

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Shoreline Change in the :>lew River Estuary, North Carolina: Rates and Consequences

Camlyn Currint *, ~cnn)' fr.l\'is\ l..i.o;a Co...,<~r t BaronH, Amit \1alhotrat , and Mar k forL..cca * ' NOAA National Ocean Sel"\oioe

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Nort."' Carolina: Ra:t<11 and ro~u~noos_ J,urtUJlQf~td. P.~eewcli, 31($), 1069---1077. Coconut Cr-wt ( Florida). ISSN 0749--0006.

AtrW ph (!tccraphy li'IU UJod l(•dttenninGrU.elof8 h<Wiinechu1p in tMNawRiver 111l1111.ryf~f'.E\ l\od1 Caro&na.from 1S56 to2004. TheN!tE llt-.oNiine "'!lldigitizo:t frorn atri.d j1'\ot£p'aph.J tilken m 1956, l!ieS, and 2004. andsh>n:line IYJ» Wall d(;((lrtni!'l&<ll by J!'(Ufld·tru!hl-og the tnlin'l &htraline by IID.lO l:oot ia 2XH .\tfjor &l'loH!line lype ea:c~\11 ib:!ludOO go;.Q.I:lpf~YeJt (fi%!if kU!),taft manih(21 *). ~ira(.d OOnlt (53\i),atd modifi«lthardened ( 19'it ~. Gn:uld-Uul.hi-lg proW:I.-rl adiD!ionald<-taill o>n relie~ a.arsh sptcietl oxnr~>o&i~CJI, and structure type. A poirU UJ&i, m(!-p-Jir.t rat.ta ppn:a:h W!JI UMd ID rr.-ure &honlifle change n::te ($Cil ) at &J m in tervs lll f<r the puicda 1~9, 1989-2001, and l !ll6-2004. ~~a.ol'lllltivewavt e:.~ (lm'eJ wu modeled f<r o,;a,c__'\ inUI'\'a.l using loeol i»th)'l'il~ ud wiad data A~r• S('R 8(ri)M all 'htf'(lir~ l)'p:l tu the entm.~ pwiod M •gtd fro!r~ -2.3to ~l .J ny 1, Wllh am ron Sf1Rof-0.3my--.l. This trarula~toar. St'(l.ftli'I ~Of....., J3mbranyo>ivl'fl~~rtht 48-~ill'p:!ri>drover00b)'t.hig n.._dy.'tb~m-:.st: n~~g&&.ive ,.....,, ag~ sen ~.p-..__._tor;t {!,._..._,) <J~Xutn.! .Jo . .., u.:vo:-g~rakd -.I..U.aoot ba.ul.. ~w•d"ll<b (-o.aJ o y ' ). Chanl!" f.lo,g m ..,.,_l &honlirt.ea(..0.18M! 1) "-AAiower t.b.9.11 alor.gMldimrlnt banks, and na n-<Mt fringingnw-;;h Ul~)tiat.ed ...-ilh Mldil'l'o(!l'lt Mn~ shorelillet l!lignificattl) rtodU'OO hlll'..k ('ll'(aioo . l\bdt~ R\-\-E valuu w-e~ po..~it lw~!y oolT't'liat:ed wih ~r.'l only in lhe hiJhtllt "-'I.VHnergyllettiJigt. ErOOoo (/lltdimmtba.'lks00relir.esprovidefl aron11trwli~&81imat.e of 1 ~.660 m3 ofaf!dinlert ea:hyear toth"enUU), o;.ith I'IUlt!lheAI!ian conltlb\;.brt;: up1DarladJiUonal l9Xlm' y-1

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Marine Corps Base Camp Lejeune

• Continuous wave recording

• 6 Hz

• 18 months

• Measured all passing vessels

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BOAT WAKE MODEL (BoMo)Boat Wake Model

V Hull [0·711) V Hul (7-1611) V Hull [16-30m)

DD Sailboat Ferryboat _j

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CSA Dcaan Sciancaa Inc.

Hull Characteristics

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Tipping point between wind wave and boat wake dominance

Comparing Wind Waves and Boat Wakes

New River ·

CSA Dcaan Sciancaa Inc.

Percentage of boat wakes exceeding wind waves

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Boat wakes and their influence o n erosion in 1he Atlantic Intracoastal Waterway,

North Carolina

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• Predicts geography of seagrass light requirements

• Informs ‘what if’ and cost-benefit questions for exploring management alternatives (scenario gaming)

• Link with wave tools for geospatial water quality forecasts

• Best application requires calibration (field assessment)

OWMo + GUI

Optical Water Quality Model (OWMo) + Graphical User Interface (GUI)

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• Slide CHL and/or TSS to see new potential habitat

• Set a depth or acreage target and see required CHL and TSS levels

OWMo – GUI interface

Works Forwards & Backwards

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Seagrass suitable area at default CHL and

TSS values

1.50 m contour

(default depth)

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1.75 m contour

1.50 m contour

(default depth)

Change in seagrass suitable area after

reducing CHL 10% and TSS 30%

New

extent

(gain)Original

extent

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SUMMARY - FORECASTING TOOLS

• Wind waves – programs forecasting wind waves and sediment movement SWAN

Delft3D

WEMo

• BoMo - forecast boat wake waves, sediment motion

• OWMo – forecast light availability using bathymetry and selective spectral attenuation

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OPPORTUNITIES

• Restoration site selection

• Seagrass cover manipulation

• Shoreline management

• Sediment resuspension forecasts

• Vessel traffic management

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ISSUES TO CONSIDER

• Not much traction with ecologists

– Historical absence of ecologist-friendly tools

– Physical assessments not taught

• Correct forecasts? Average conditions vs Extremes

– Extent

– Resolution

– Duration

– Intensity

– Return interval (1/frequency)

– Sequence

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Questions?

Waves, Wakes and Water Clarity: Understanding Physical Drivers of Seagrass Distribution in Coastal Waters

Mark Fonseca, Ph.D.CSA Ocean Sciences Inc.

Amit Malhotra, MSc., GISPGeohorizons

Page 22: Waves, Wakes and Water Clarity - lwli.org WEMo • BoMo - forecast boat wake waves, sediment motion • OWMo –forecast light availability using bathymetry and ... Waves, Wakes and

Questions?