tidal rectification = overtides and compound tides nonlinear effects on tides
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Tidal Rectification = Overtides and compound tides
Nonlinear effects on tides
From Parker (2007)
simple sine wave
asymmetry between flood and ebb
double low waters
extreme distortion: tidal bore
From Parker (2007)
HgC
88
77
55
66
11
2233
44
Nonlinear effects in estuaries
(Parker, 1991, Tidal Hydrodynamics, p. 247)
We will talk mainly about nonlinear tidal interactions
Consider the tide: tuu ii
i cos0
tututuu MMMMMM 222222
22000
2 coscoscos
tu MM 22
2cos1212
0
tuuxu
u
M
MMM 4
2222cos
21
21
α 20
f(t)not residual
20
42 h 21.62
h 42.122
22 MM
overtide
And the nonlinear term 2
21
uxx
uu
and i = M2 only
If M2 interacts with S2:
coscoscoscos
days 4.81 modulation freqlow
h 1.6 distortion freq high
0000 2222222222ttuututu SMSMSMSSMM
days 8.14)0177.0)(24(
2 ;0177.0
122
42.122
.,.22
Tei SM
Nonlinear interactions also arise from bottom friction, which yields: η u|u| and u|u|
and from the divergence term in the continuity equation, which is proportional to η u
0 1
uHbxbt
(one dimensional, vertically and laterally integrated equation; b is estuary’s breadth)
We then have four mechanisms that generate nonlinearities:
uuDuuCxu
uBux
A ); ); ); )
H
uuC
xg
xu
utu
bGenerating mechanisms arise from
uuD
uuCxu
uB
ux
A
)
; )
; )
; )
H
uuC
xg
xu
utu
bGenerating mechanisms arise from
Nonlinear terms on tidal constituents effect a modulation and a distortion of that constituent
M2 - x M2 + x 2 M2 - x 2 M2 + x 4 M2 - x
M2 Residual M4 - M6 M6
(12.42 h) - (6.21 h) - (4.14 h) (4.14 h)
N2 MN (Mm) MN4 2MN2 2MN6 4MN6
(12.66 h) (27.3 d) (6.27 h) (12.19 h) (4.17 h) (4. 11 h)
S2 MS (MSf) MS4 2MS2 ( 2) 2MS6 4MS6
(12 h) (14.8 d) (6.10 h) (12.87 h) (4.09 h) (4.19 h)
K1 MK1 (O1) MK3 2MK3 2MK5 4MK7
(23.93 h) (1.07 d) (8.17 h) (8.38 h) (4.93 h) (3.57 h)
O1 MO1(K1) MO3 2MO3 2MO5 4MO7
(25.82 h) (0.99 d) (8.38 h) (8.17 h) (5 h) (3.52 h)
1-1 1+1 2-1 2+1 4-1
even even odd odd odd
Mech A, B, C, D A, B, C,D D D D
M2 + x 2 M2 + x
M4 M6
Interactions of M2 with other constituents
generate constituents with the following frequencies:
σM2 - σx σM2 + σx 2σM2 - σx 2σM2 + σx 4σM2 - σx
M2 Overtides
M2 interactions with overtides
symmetric distortionsymmetric distortion(by odd harmonic)(by odd harmonic)
asymmetric distortionasymmetric distortion(by even harmonic)(by even harmonic)
Rectified Tide
Rectified Tide
Physical explanation for nonlinear interactions
For long waves without friction, the wave propagation velocity C is [ g H ]½
This is approximately constant throughout the tidal cycle, only if the tidal amplitude η << H, i.e., if η / H << 1
In reality, η / H is not much smaller than 1 and the wave crest will travel faster (progressive wave in shallow water) than the trough, resulting in:
energy at M4 frequency
This is the asymmetric effect of the nonlinear continuity term (mechanism A)
) ux
A
Difference between Difference between sinusoid and distorted sinusoid and distorted wave yields energy in wave yields energy in the 2the 2ndnd harmonic harmonic
The tidal current amplitude may be approximated as:
xg
dtdu
xu
dtd
H
txaCg
utxa
CH
u
1
)sin()sin(
0
This is the effect of the inertial term:
)xu
uB
ebb
flood
For η / H > 0.1, u is not negligible with respect to C (as it usually is).
Then, the wave propagation velocity at the crest is C + u0
and the wave propagation velocity at the trough is C - u0
which results in a similarly distorted wave profile(tidal wave interacting with tidal current):
CC – – uu00
CC + + uu00
Frictional loss of momentum per unit volume is greater at the trough than at the crest.
Then, crest will travel faster than the trough; will generate asymmetric distortion andeven harmonics (M4)
H
uuC
xg
xu
utu
bGenerating mechanisms arise from
Quadratic friction u| u | causes a symmetric distortion, i.e., maximum attenuation at maximum flood and at maximum ebb; minimum attenuation at slack water. This will generate an odd harmonic (M6)
Therefore, there are symmetric effects and asymmetric effects
Asymmetric Effects
morevslessuu
uCvsuCxu
u
HgCvsHgCux
00
)()(
generate even harmonics (e.g. M4) because max C and minimum attenuation occurs at crest
Symmetric Effects
u | u | extreme attenuation at flood and ebb, and minimum attenuation at slack waters
Produce odd harmonics, e.g., M6 because there are 3 slack waters and two current maxima in one period
symmetric symmetric distortiondistortion(by odd (by odd harmonic)harmonic)
asymmetric asymmetric distortiondistortion(by even (by even harmonic)harmonic)
Effects of a mean flow (e.g. River Flow)
Can be explained in terms of changes in C and frictional attenuation (u | u | )
Mean river flow makes ebb currents stronger increased frictional loss flood currents weaker decreased frictional loss
This results in greater energy loss than if the river flow was not present,which translates into:
reduced tidal rangegreater damping of tidal wave
Friction will now produce asymmetric effects and generation of M4
Frictional generation of M6 will continue as long as uR < u0 so that there are still slack waters
greatestattenuation
t
Flood
Ebb
Attenuation
When uR > u0
Flow becomes unidirectional (no more slack waters) and no generation of odd harmonics
t
Flood
Maximum attenuation
Ebb
Minimum attenuation
u
t
Flood
Ebb
Attenuation
Ebb
Flood
Current velocity data near Cape Henry, in the Chesapeake Bay
January 20-June 9, 2000
σM 2 - σx σM 2 + σx 2 σM 2 - σx 2 σM 2 + σx 4 σM 2 - σx
M 2 R esid ual M 4 - M 6 M 6
(1 2.42 h) - (6 .21 h) - (4 .14 h) (4 .14 h)
N 2 M N (M m) MN 4 2MN 2 2MN 6 4MN 6
(1 2.66 h) (2 7.3 d ) (6 .27 h) (1 2.19 h) (4 .17 h) (4 . 1 1 h)
S 2 M S (MS f) MS 4 2 M S 2 (µ 2) 2 M S 6 4 M S 6
(1 2 h) (1 4.8 d ) (6 .10 h) (1 2.87 h) (4 .09 h) (4 .19 h)
K 1 M K 1 (O 1) MK 3 2MK 3 2MK 5 4MK 7
(2 3.93 h) (1 .07 d ) (8 .17 h) (8 .38 h) (4 .93 h) (3 .57 h)
O 1 M O 1(K 1) MO 3 2MO 3 2MO 5 4MO 7
(2 5.82 h) (0 .99 d ) (8 .38 h) (8 .17 h) (5 h) (3 .52 h)
1 -1 1 +1 2 -1 2 + 1 4 -1
e ve n e ve n o dd o dd o dd
M e c h A, B, C A, B, C C C C
σM 2 - σx σM 2 + σx 2 σM 2 - σx 2 σM 2 + σx 4 σM 2 - σx
R esid ual M 4 - M 6 M 6
σM2 - σx σM2 + σx 2σM2 - σx 4σM2 - σx
Spectrum for current velocity at Ponce de Leon Inlet
Spe
ctra
l ene
rgy
(m2 /
s2 /cp
d)
Cycles per day
Ensenada de la Paz
Example of Overtides and Compound Tides
More evidence sought from
time series with Moored Instruments
Early March to Early May 2003
Power spectrum of Principal-axis ADCP bins
Appreciable overtides and compound tides – tidal rectification
O1,K1 N2,M2,S2
MK3,2MK3
M4
2MK5,2MO5
M6
4MK7,4MO7
ADCP pointing downward1-m bins recorded for ~2.5 days, i.e., ~ 5 cyclesDecember 14.5 to 17, 2004Deployed just seaward of bar