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Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

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Page 1: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Temporal Variability in an Estuary:Keeping it Linear

Jim Lerczak

Woods Hole Oceanographic Institution

PhD 1995-2000

Page 2: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Myrl with studentCirca 1998

Page 3: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Rick Salmon

Geophysical Fluid Dynamics teacher extraordinaire

Shares Myrl’s gift for clarity and eloquence

Page 4: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Dave Chapman

First met at OS 2000

Post-doctoral mentor

Page 5: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Two Lessons Learned from Myrl

ILS Institute forLinear Science

2) Choose field sites with easyaccess to fine dining

1) Start with linear analyses,even when the underlyingdynamics are far from linear.

Page 6: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

6

22

33

43

55

75

0

Field Work Here

Wine/DineHere

Hudson RiverEstuary 2004

Page 7: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

River Discharge(m3s-1)

Tidal Amplitude(m/s)

EstuaryLength (km)

Decimal Days (2004)

Page 8: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Salt Balance in an (Exchange Dominated) Estuary

Ocean(salty)

River(f resh)

TidalTurbulent

Mixing

EstuarineCirculation

FluxSaltDrivenExchangeSQdt

ContentSaltdf o

Qf

Salt Flux due to Baroclinic Exchange Flow:

Fe = ∫ueSedA ~ H Δu ΔS

x

S

x

SHg

2

3

82

eF

• ∂S/∂x ≈ So/L

• κ ~ UT

• Linearize about mean estuary length, mean tidal amplitude and mean discharge

L = Lo + L’

Qf = Qo + Q’

UT = UTo + UT’

oo3

11

T

To

U

U

Q

QLL

dt

Ld

o

o

6Q

AL

3

1

o3

o

82o

o

Q

AHSgL

Page 9: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Linear Response to Sinusoidal ForcingSpring-Neap Cycle (period = 14.8 days)

τ/Tf

0 1 2 3

Res

pons

e am

plit

ude

|L‘|

/ aL

o

0

0.5

1

Pha

se L

ag, φ

(deg

rees

)

0

45

90

221

1

atan

f = sin(ωt)

L'/

Loa

0

1

-1

Time, t0 1 2

τ/Tf = 0.1

τ/Tf = 1

τ/Tf = 3

a)

b)

Page 10: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

τ = 14.8 days

Large spring-neap response

Weak spring-neap response

Theoretical LinearResponse Time

Res

pons

e T

ime

Fro

m M

odel

Fit

Model Fit of Response Time

Page 11: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Equilibrium Estuary Lengthfor Mean Tidal Conditions

Equ

ilibr

ium

Len

gth

(km

)

Mean Freshwater Discharge (m3s-1)

Page 12: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Lo

Time-DependentSpring-Neap Range

22o1

45.01

L

22o1

45.01

L

Steady Neap LengthLo(1 + 0.45)

Steady Spring LengthLo(1 - 0.45)

Summary of Linear Analysis

Page 13: Temporal Variability in an Estuary: Keeping it Linear Jim Lerczak Woods Hole Oceanographic Institution PhD 1995-2000

Na zdrowie, Myrl

• Thanks for your intellectual enthusiam (for oceanography and beyond).

• Thanks for your friendship.

• Thanks also to Art! for organizing the first meeting of the M.H. Fan Club