View
215
Download
1
Tags:
Embed Size (px)
Citation preview
Temporal Variability in an Estuary:Keeping it Linear
Jim Lerczak
Woods Hole Oceanographic Institution
PhD 1995-2000
Myrl with studentCirca 1998
Rick Salmon
Geophysical Fluid Dynamics teacher extraordinaire
Shares Myrl’s gift for clarity and eloquence
Dave Chapman
First met at OS 2000
Post-doctoral mentor
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.
6
22
33
43
55
75
0
Field Work Here
Wine/DineHere
Hudson RiverEstuary 2004
River Discharge(m3s-1)
Tidal Amplitude(m/s)
EstuaryLength (km)
Decimal Days (2004)
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
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)
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
Equilibrium Estuary Lengthfor Mean Tidal Conditions
Equ
ilibr
ium
Len
gth
(km
)
Mean Freshwater Discharge (m3s-1)
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
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