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Tidal asymmetry and residual sediment transport in estuaries

Authors:
Tidal asymmetry
and residual
sediment
transport in
estuaries
Z. B. Wang, C. Jeuken, H.J. de Vriend
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics i
Contents
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics ii
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Appendices
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 1–1
1 Introduction
1.1 Background
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 1–2
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1.2 Objective of the study
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1.3 Set up of the study
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1.4 Acknowledgement
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–1
2 General Theory
2.1 General
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–2
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2.2 Basic theory
2.2.1 Introduction
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–3
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2.2.2 Tidal asymmetry
Locally generated overtides (1-D)
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–4
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–5
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–6
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–7
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–8
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2.3 Analysis of relevant aspects
2.3.1 Mechanisms determining asymmetry of horizontal tide
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–9
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–10
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2.3.2 Asymmetry of horizontal tide and vertical tidal constituents
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Tidal asymmetry and tidal constituents of the vertical tide
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A<-="( 39;;"&"2#"( %"8D""2( 8<"( 0:"&893"( -23( 8<"( ="$9P391&2-E( 893"+( H-."( ;0&( "V-$AE"( 8<"
-=>$$"8&>(#-1="3(%>(8<"(U1-&8"&P391&2-E(893"+(_E003P30$92-2#"(\D-8"&(E":"E(&9="=(;-=8"&(8<-2
98( ;-EE=^( 0##1&=( 9;( 8<"( A<-="( 39;;"&"2#"( 9=( %"8D""2( L0( -23( )IL0'( 08<"&D9="( "%%P30$92-2#"
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_9/+5+5(@#<"$-89#(#&0==P="#8902(1="3(%>(,002(\)*II^
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–11
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–12
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–13
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–14
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–15
G8(9=(#E"-&(8<-8(-=>$$"8&>(92(8<"(:"&89#-E(893"(D9EE(39&"#8E>(#-1="(-=>$$"8&>(92(8<"(<0&9K028-E
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2.3.3 Relations between morphology and tidal asymmetry
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Influence of morphology on tidal asymmetry
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–16
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–17
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–18
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–19
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–20
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–21
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 2–22
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–1
3 Tidal asymmetry in the Western Scheldt
3.1 Introduction
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–2
3.2 Description Western Scheldt
3.2.1 Hydrodynamics
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3.2.2 Morphology
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–3
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–4
Vak 1
0
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Vak 4
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Vak5
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–5
Vak 1
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100
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Vak 2
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100
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Vak 4
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100
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–6
3.3 Mechanisms generating tidal asymmetry
3.3.1 Residual flows
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–7
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–8
3.3.2 Relation between asymmetries in vertical and horizontal tide
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–9
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–10
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–11
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–12
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–13
M2 flood channel
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
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M4 flood channel
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0.4
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0.8
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M6 flood channel
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0.2
0.4
0.6
0.8
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M2 ebb channel
-0.8
-0.6
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0.4
0.6
0.8
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0.2
0.4
0.6
0.8
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M6 ebb channel
-0.8
-0.6
-0.4
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0.4
0.6
0.8
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–14
3.4 Temporal variation of the asymmetry of the vertical tide
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–15
Vlissingen
-0.5
0
0.5
1
1.5
2
2.5
0 5 10 15 20 25 30 35 40 45
lunar day
a0, a2 (m)
0
0.05
0.1
0.15
0.2
0.25
a4, a6 (m0
a0
a2
a4
a6
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Vlissingen
0
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0 5 10 15 20 25 30 35 40 45
lunar day
amplitude ratio
0
0.5
1
1.5
2
2.5
a2(m)
a4/a2
a6/a2
a2
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–16
H<9=(E"-3=(80(8<"(#02#E1=902(8<-8(=0$"(0;(8<"(:-&9-8902(#<-&-#8"&9=89#=(0;(8<"(893-E(-=>$$"8&>
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Vlissingen
0
0.02
0.04
0.06
0.08
0.1
0.12
0.14
1.2 1.4 1.6 1.8 2 2. 2 2.4
a2 (m)
a4/a2
Vlissingen
0
0.02
0.04
0.06
0.08
0.1
0.12
1.2 1.4 1.6 1.8 2 2.2 2.4
a2 (m)
a6/a2
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Vlissingen
-40
-20
0
20
40
60
80
100
120
1.2 1.4 1.6 1.8 2 2.2 2.4
a2(m)
2φ2−φ4
2φ2−φ42φ2−φ4
2φ2−φ4
Vlissingen
50
60
70
80
90
100
110
1.2 1.4 1.6 1.8 2 2.2 2.4
a2(m)
3φ2−φ6
3φ2−φ63φ2−φ6
3φ2−φ6
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–17
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=1=#"A89%E"(80((E-&/"("&&0&=(92(8<"(893-E(-=>$$"8&>(31"(80(8<"(0:"&893"=`
!" e9#.92/(-2(-&%98&-&>(89$"P928"&:-E($"-2=(#<00=92/(-(A0928(92(8<"(D93"(=#-88"&(0;(_9/+
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92(8<"(<-E;P#>#E"(;&0$(;&0$(2"-A(80(=A&92/(0&(;&0$(=A&92/(80(2"-A'(98(-E=0(3"A"23=(02
8<"(21$%"&(0;(893-E(#02=8981"28=(1="3+
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&"=1E8=(0;(8<"(_01&9"&(-2-E>=9=(;0&(-2(-&%98&-&9E>(="E"#8"3(89$"P928"&:-E+
3.5 Relation between tidal asymmetry and morphology
C( ;9&=8( 39=#1==902( 02( 8<"( &"E-8902( %"8D""2( 8<"( $0&A<0E0/9#-E( 3":"E0A$"28( -23( 8<"
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&"=1E8=(92(8<"(E98"&-81&"'("+/+(8<0="( 0;( @A""&("8( -E( \)**)^'(-&"(U1-E98-89:"E>(-AAE9#-%E"(80( 8<"
R"=8"&2(@#<"E38'("=A"#9-EE>(D<"2(8<"(#<-2/"(0;(8<"(893-E(-=>$$"8&>(9=(#02=93"&"3+
G2(8<"(A&"="28(="#890$'(8<"(92;E1"2#"(0;($0&A<0E0/9#-E(#<-&-#8"&9=89#=(02(8<"(893-E(-=>$$"8&>
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-&"-=( 8"23( 80( %"( "%%P30$92-28( -23( &"E-89:"E>(=<-EE0D( "=81-&9"=( 8"2 3( 80( %"( ;E003P30$92-28+
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8<-8(-&"(9$A0&8-28(;0&(8<"(893-E(-=>$$"8&>(92(8<"(R"=8"&2(@#<"E38a
3.5.1 Tidal asymmetry with respect to quarter-diurnal tide
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C( 39=#1==902(0;( 8<"( 3":"E0A$"28(=<0D2( %>( 8<9=( ;9/1&"( 9=( /9:"2( %>( F"&&98="2( "8( -E( \)***^+
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-=>$$"8&>( -8( -( #"&8-92( =8-8902( 9=( 928"&&"E-8"3( D98<( 8<"( 893-E( -=>$$"8&>( 92( 8<"( 30D2=8&"-$
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–18
\="-D-&3^(E0#-8"3(-&"-+(,-="3(92(8<9=(A&"=1$A8902(98( 9=( <>A08<"=9="3( ( 8<-8(!4*&74$/?*&-,&!4*
!"#$%& $'())*!+(& "/& $& 7*+!$"/& 2$+!& -,& !4*& *'!1$+(<& +$!4*+& !4$/& !4*& !"#$%& $'())*!+(& "!'*%,<
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*'!1$+(3(H<9=(<>A08<"=9=(D9EE(%"(1="3(-=(/193"E92"(92(8<"((-2-E>=9=(%"E0D+
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A-&-$"8"&=(-&"(8<1=(3";92"3(-=
a
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21
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:9=9%E"(8<-2(92(_9/+?+)L+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–19
_&0$((;9/1&"(?+))(=<0D=(8<"(;0EE0D92/(;"-81&"=(&"/-&392/(8<"(-=>$$"8&>(0;(8<"(:"&89#-E(893"
92(8<"(8<&""(&"/902=(0;(8<"("=81-&>`
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;E003( 30$92-28+( H<9=( 9=( 9239#-8"3( %>( 8<"( A0=989:"( :-E1"( 0;( 8<"( A<-="P39;;"&"2#"
A-&-$"8"&( ,-8<PS-2=D""&8(\1AA"&( A-2"E^+( H<"( 3"#&"-="( 0;( 8<9=( A-&-$"8"&( %"8D""2
)*T)(-23()*IL'(A0928=(-8(-(&"31#8902(0;(8<9=(;E003(30$92-2#"(92(89$"+(H<"(-$AE9813"
&-890(A-&-$"8"&(92989-EE>(3"#&"-="3(-23(9=(92#&"-=92/(-/-92(=92#"(-%018()*IL+
0.05
0.055
0.06
0.065
0.07
0.075
0.08
1970 1975 1980 1985 1990 1995 2000
Amplitude ratio M4/M2
vlissingen
terneuzen
hansweert
bath
-30
-20
-10
0
10
20
30
1970 1975 1980 1985 1990 1995 2000
yea r
phase differnce 2M2-M4
Vlissingen
Terneuzen
Hansweert
Bath
_9/?+)L(!":"E0A$"28(0;((8<"(-$AE9813"(&-890(-23(A<-="(39;;"&"2#"(%"8D""2(8<"(J5(-23(JB
893"+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–20
!" H<"(#"28&-E( A-&8(0;(8<"("=81-&>'(%"8D""2(H"&2"1K"2(-23(S-2=D""&8(\]-.(?(-23(B^'(9=
"%%P30$92-28+(H<"("%%P30$92-2#"(92(8<9=(-&"-(3"#&"-="3(%"8D""2()*T)(-23()*IN+
!" G2(8<"(D"=8"&2(A-&8(0;(8<"("=81-&>'(%"8D""2(]E9==92/"2(-23(H"&2"1K"2(\]-.(N(-23(Q^'
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30$92-28(31&92/(8<"(A"&903()*T)P)**T+
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%13/"8(=8139"=+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–21
3.5.2 Morphological characteristics and their changes
m=92/(8<"( 92;0&$-8902(0;(8<"(<>A=0$"8&>(-=(3"=#&9%"3( 92(="#8902(?+5(98( 9=( A0==9%E"( 80(3"&9:"
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0.8
0.85
0.9
0.95
1
1.05
1.1
1970 1975 1980 1985 1990 1995 2000
amplitude parameter
terneuz en
hansweert
bath
-25
-15
-5
5
15
25
35
45
55
1970 1975 1980 1985 1990 1995 2000
phase parameter
terneuzen
hansweert
bath
_9/+?+))(!":"E0A$"28(0;(8<"(&"E-89:"(-$AE9813"(-23(A<-="(A-&-$"8"&=(\"U+(?+)I^+(M"E-89:"
&";"&=(80(8<"(#<-2/"=(D98<(&"=A"#8(80(8<"(="-D-&3(E0#-8"3(D-8"&(E":"E(=8-8902'(9+"H"&2"1K"2
:"&=1=(]E9==92/"2'(S-2=D""&8(:"&=1=(H"&2"1K"2(-23(,-8<(:"&=1=(S-2=D""&8+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–22
_0&(]='(8<"(:0E1$"(0;(D-8"&(=80&"3(02(893-E(;E-8(%"8D""2(<9/<(-23(E0D(D-8"&'(D"(<-:"
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VVaVa Faa
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a
h
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da
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α
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11
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()
V
V
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d
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d
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d
a
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da
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)**Q(-&"(=<0D2(92(8<"(E";8(A-2"E(0;(_9/+?+)5+(G2(8<"(&9/<8(A-2"E(8<"(;E003P(-23("%%P30$92-2#"
0;(8<"(:"&89#-E(893"(92(8<"(=9V(-&"-=(9=(9239#-8"3+(H<"(E-88"&(92;0&$-8902(9=(0%8-92"3(;&0$(;9/1&"
?+))(\=""(A&":901=^(="#8902+(_0&(8<"($0&A<0E0/9#(=981-8902(0;( )*NN( 8<"((893-E( -=>$$"8&>( 92
)*T)( 9=( 9239#-8"3( =92#"(92;0&$-8902(0;( 8<"( 893-E(-=>$$"8&>(9=( 208( -:-9E-%E"( ;0&()*NN+( H<9=
E"-3=(80(8<"(;0EE0D92/(0%="&:-8902=([(#02#E1=902=`
!" J0=8(;E003(30$92-28(A-&8=(0;(8<"("=81-&>(<-:"(E-&/"&(:-E1"=(0;(-[<(-=(D"EE(-=(]=[]#+
H<"(;-#8(8<-8(E-&/"&(:-E1"=(0;(-[<(#0&&"=A023( D98<( ;E003P30$92-2#"(-/&""=( D98<(8<"
#02#E1=902=(0;(@A""&("8(-E(\)**)^+(q1-E98-89:"E>(8<"(&"=1E8=(0;(@A""&("8(-E+(\)**)^(-&"
8<1=(-AAE9#-%E"(80(8<"(R"=8"&2(@#<"E38+(S0D":"&'(8<"("V-#8(="A-&-80&((%"8D""2("%%P
30$92-2#"(-23( ;E003P30$92-2#"( -=( =<0D2( 92( _9/+?+)5( 9=( 208( 8<"(=-$"( -=( 8<"( 02"
;0123(%>(@A""&("8(-E+\)**)'(=""(_9/+5+*^+(H<9=(D-=(80(%"("VA"#8"3'(=92#"(8<"(R"=8"&2
@#<"E38(39;;"&=(:"&>($1#<(;&0$(8<"("=81-&9"=(#02=93"&"3(%>(_&9"3&9#<=("8(-E+(\)**L^+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–23
!" H<"&"( 9=( 02"( A0928( ( 92( 8<"( &9/<8( A-2"E( ( 8<-8( ( 3":9-8"=( ;&0$( 8<"( /"2"&-E( 8&"23+( G8
&"A&"="28=(8<"(A-&8(]-.(N(92()**Q+(H<9=(-&"-(9=(=A"#9;9"3(-=(;E003P30$92-28(%"#-1="'
-##0&392/(80(_9/+?+))'92()**Q(8<"(D"=8"&2(A-&8(\]-.(N( -23( Q^( =<0D=( -(=E9/<8(;E003P
30$92-2#"( -23( %"#-1="( ]-.( N( <-=( -( E-&/"&( -[<( :-E1"( 8<-2( ]-.( Q+( G2( ;9/+?+)5( 8<9=
A0928(9=(E0#-8"3(92(-(&"/902(D<"&"(-EE(08<"&(A0928=(-&"("%%P30$92-28(+(H<"(#02#E1=902
9=( 8<"&";0&"( 8<-8( 8<"( 8<"0&>( 0;( @A""&( "8( -E( \)**)^( ( 30"=( 208( "VAE-92( 8<"( ;E003P
30$92-2#"(0;(8<"(D"=8"&2(A-&8(0;(8<"("=81-&>(92()**Q+
H<"(-2-E>=9=(#-2(-E=0(%"(8-."2(02"(=8"A(;1&8<"&(%>(&"E-892/(8<"(#<-2/"=(0;(8<"($0&A<0E0/>(80
8<"(#<-2/"=(0;(8<"(893-E(-=>$$"8&>+(_0&(8<9=(A1&A0="(8<"(39;;"&"2#"=(0;(8<"(8D0(A-&-$"8"&=(92
8<"(8D0(>"-&=(\)*NN( -23()**Q^( -&"( &"E-8"3(80( 8<"( #<-2/"(0;( 893-E(-=>$$"8&>(;&0$()*T)( 80
)**T(\_9/+?+)?^+(_9&=8(8<"(8D0(A-&-$"8"&=(-[<(-23(]=[]#(-23(8<"9&(#<-2/"=(;&0$()*NN(80()**Q
-&"(3"8"&$92"3(;0&(8<"(=9V(A-&8=(\8<"(1AA"&(A-2"E=(0;(_9/+?+)?^+(H<"2(8<"(-:"&-/"(#<-2/"=(0;
8<"(8D0(A-&-$"8"&=(92(8<"("-=8"&2(A-&8(\-:"&-/92/(]-.()(-23(5^'(8<"(#"28&-E(A-&8(\]-.(?(-23(B^
-23( 8<"( D"=8"&2( A-&8( \]-.( N( -23( Q^( -&"( &"E-8"3( 80( 8<"( #<-2/"(0;( 8<"( A<-="( 39;;"&"2#"(;&0$
)*T)( 80( )**T( -=( =<0D2( 92( _9/+?+))( \8<"( E0D"&( A-2"E=( 0;( _9/+?+)?^+( H<"( ;0EE0D92/
0%="&:-8902=(-&"($-3"`
!" J0=8(#<-2/"=(0;(8<"(8D0(A-&-$"8"&=(0##1&(92(8<"("-=8"&2( A-&8( 0;(8<"("=81-&>(\]-.()
-23(5^+
!" H<"(#<-2/"(0;(8<"(8D0(A-&-$"8"&=(=""$(80(%"(&"E-8"3(D98<("-#<(08<"&+
!" H<"( #<-2/"( 0;( %08<( A-&-$"8"&=( #0&&"E-8"=( D"EE( D98<( 8<"( #<-2/"( 0;( 8<"( 893-E
-=>$$"8&>(92(8<"(#0&&"=A02392/(A-&8+
H<-8(8<"(#<-2/"=(0;(8<"(8D0(A-&-$"8"&=(=""$(80(%"(&"E-8"3(D98<("-#<(08<"&(9=(31"(80(8<"(;-#8
8<-8(-[<( -23(]=[]#( -&"( 208(923"A"23"28(0;( "-#<(08<"&+(H<9=(9=( =9$AE>( 9EE1=8&-8"3(%>( 8<"( ;-#8
8<-8(-2(92#&"-="(0;(893-E(-$AE9813"'(;0&("V-$AE"'(#-1="=(-2(92#&"-="(92(%08<(A-&-$"8"&=+(G2(8<"
A&"="28(#-="'(8<"(#<-2/"=(0;(%08<(A-&-$"8"&=( -&"( $-92E>(#-1="3(%>(8<"(#<-2/"=(92( 8<"(3""A
#<-22"E( A-&8='( -=( 9=( =<0D2( 92( _9/+?+)BP_9/+?+)Q+( H<"( ;9/1&"=( /9:"( ( 8<"( :0E1$"( #<-2/"=( 0;
:-&901=(A-&8=(0;(8<"("=81-&>(;&0$()*NN(80()**Q+
0
0.01
0.02
0.03
0.04
0.05
0.06
0.07
0.08
0.09
0.1
0 0.05 0.1 0.15 0.2 0.25
a/h
Vs/Vc
flood-dominant
ebb-dominant
0
0.01
0.02
0.03
0.04
0.05
0.06
0.07
0.08
0.09
0.1
0 0.05 0.1 0.15 0.2 0.25
a/h
Vs/Vc
1955
1996
_9/+?+)5(H<"(/"0$"8&9#(A-&-$"8"&=(92(8<"(=9V(A-&8=(0;(8<"(R"=8"&2(@#<"E38(92()*NN(-23()**Q
\E";8^(-23(92(&"E-8902(80(8<"(;E003("%%P30$92-2#"(0;(8<"(:"&89#-E(893"(\&9/<8^
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–24
q1-E98-89:"E>(8<"( 8<"0&>(0;(@A""&( "8( -E( \)**)^'( -E8<01/<(%-="3( 02(808-EE>(39;;"&"28(#-="='(9=
A"&;"#8E>(-AAE9#-%E"( 80("VAE-92( 8<"( #<-2/"=( 0;(8<"( -=>$$"8&>(0;(:"&89#-E(893"( 92(8<"( R"=8"&2
@#<"E38'(#-1="3(%>(8<"(U1-&8"&P391&2-E(893"+
0
0.05
0.1
0.15
0.2
0.25
va k 1 va k 2 va k 3 va k 4 va k 5 va k 6
a/h
1955
1996
1971-1996
-40
-30
-20
-10
0
10
20
-0.04 -0.03 -0.02 -0.01 0 0.01
change of a/h
change of 2φ2−φ4
2φ2−φ42φ2−φ4
2φ2−φ4
0
0.01
0.02
0.03
0.04
0.05
0.06
0.07
0.08
0.09
va k 1 va k 2 va k 3 vak 4 va k 5 vak 6
Vs/Vc
1955
1996
1971-1996
-40
-30
-20
-10
0
10
20
-0.04 -0.03 -0.02 -0.01 0 0.01
change of Vs/Vc
change of 2φ2−φ4
2φ2−φ42φ2−φ4
2φ2−φ4
_9/+?+)?(W<-2/"=(0;(8<"(8D0($0&A<0E0/9#-E(A-&-$"8"&=(-=(3";92"3(%>(@A""&("8(-E(\)**)^(-23
8<"9&(&"E-8902(80(8<"(#<-2/"=(0;(8<"(&"E-89:"(A<-="(39;;"&"2#"(%"8D""2(JB(-23(J5
_9/+?+)B(]0E1$"(#<-2/"=(0;("-=8"&2(A-&8(0;(R"=8"&2(@#<"E38(\]-.()(-23(5^
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–25
3.5.3 Other indicating parameters
T!4*+&$%!*+/$!"6*'
G2=8"-3(0;(8<"(8D0(A-&-$"8"&=(\-[<(-23(]=[]#^(3";92"3(%>(@A""&("8(-E+(\)**)^(8<"(-AAE9#-8902
0;(08<"&(-E8"&2-89:"(A-&-$"8"&=(#-2(%"(#02=93"&"3`
_9/+?+)N(]0E1$"(#<-2/"=(0;(8<"($933E"(A-&8(\]-.(?^
_9/+?+)Q(]0E1$"(#<-2/"=(92(8<"(D"=8"&2(A-&8(\]-.(B'(N(-23(Q^
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–26
!" N%40&!B1&180%0&7! ?')$(!+$! 2+%0&1%)&0,( C=(3 "=#&9%"3( 92( W<-A8"&( 5'( 8<"&"( -&"( -E=0
08<"&( A-&-$"8"&=( =1//"=8"3( 92( 8<"( E98"&-81&"+( C2( "V-$AE"( 9=( 8<"( 02"( =1//"=8"3( %>
!&02."&=(\)*IQ'(="#8902(5+?+?^+(C(=9$9E-&(-2-E>=9=(-=(3"=#&9%"3(-%0:"(#-2(%"(#-&&9"3
018(;0&(8<9=(A-&-$"8"&+(H<"(#02#E1=902=(D9EE(%"(=9$9E-&(80(8<0="(3&-D2(;0&(8<"(8<"0&>
0;( ( @A""&( "8( -E+( \)**L^+( H<9=( #-2( =9$AE>( %"( 0%="&:"3( %>( #0$A-&92/( _9/+?+)5( -23
_9/+5+)L+
!" O7+$P!+$(0B0$(0$%!B1&180%0&7,(C=($"28902"3(92(8<"(A&":901=(=1%P="#8902'(8<"(8D0
A-&-$"8"&=(3";92"3(%>(@A""&("8(-E(\)**)^(-&"(208(923"A"23"28(0;("-#<(08<"&+(H<9=(#-2
%"( -( 39=-3:-28-/"+(C( A0==9%E"( ="8( 0;( 923"A"23"28( A-&-$"8"&=( #028-9292/( 8<"( =-$"
92;0&$-8902( 9=( "+/+( -[<( -23( C;[C'( D<"&"( 8<"( E-=8( A-&-$"8"&( &"A&"="28=( 8<"( &-890
%"8D""2(8<"(<0&9K028-E(-&"-(0;(893-E(;E-8=(-23(8<"(808-E(-&"-(0;(8<"(#0&&"=A02392/(\A-&8
0;^( "=81-&>+( G8( 9=( &"#0$$"23"3( 80( #02=93"&( 8<9=( ="8( 0;( A-&-$"8"&=( 92( 8<"( ;0EE0D92/
=813>
!" 340!B1&180%0&7!+$! %40! ?+%%+$P! 0F)1%+'$!?'&!%40!45B7'80%&5,(G2(#0$%92-8902( D98<
8<"( 893-E( -$AE9813"( 8D0( 39$"2=902E"==( A-&-$"8"&=( /( -23( -[3( #-2( %"( 3";92"3+( H<"
=-$"(3-8-(-=(92(_9/+?+)5(20D(>9"E3(_9/1&"(?+)T+(G8(=""$=(8<-8(8<9=(="8(A-&-$"8"&=(<-=
8<"( A08"289-E( 80( ="A-&-8"( 8<"( ;E003P30$92-28( -&"-=( ;&0$( 8<"( "%%P30$92-28( 02"=+
S0D":"&(8<"&"(9='(20(8<"0&"89#-E(%-=9=(;0&(98(-8(8<9=($0$"28(\8<"(="A-&-80&(E92"(3&-D2
92( 8<"( ;9/1&"( 9=( -( =1//"=89:"( 02"^+( _1&8<"&$0&"'( 8<9=( ="8( 0;( A-&-$"8"&=( <-=( 98=
&"=8&9#8902='(=92#"( 98(#-2( 02E>(%"(1="3( 92( #-="=(D<"&"(8<"(=1//"=8"3(;98892/("U1-8902
;0&(8<"(<>A=0$"8&>(-AAE9"=+
I##"!"-/$%&2$+$)*!*+'
H<"(;-#8(8<-8(8<"(8<"0&9"=(;0123(92(8<"(E98"&-81&"(-&"(208(U1-2898-89:"E>(:-E93(;0&(8<"(R"=8"&2
@#<"E38( 9239#-8"=( 8<-8( "+/+( 8<"( A-&-$"8"&=( 3";92"3( %>( @A""&( "8( -E+( \)**)^( 30( 208( ;0&$( -
#0$AE"8"(="8('(92(8<-8(8<">(#0:"&(-EE(&"E":-28(-=A"#8=(0;(8<"(893-E(-=>$$"8&>(92(8<"("=81-&>+(G2
08<"&( D0&3='( 8<"&"( $1=8( %"( 08<"&( A-&-$"8"&=( D<9#<( -E=0( <-:"( 92;E1"2#"( 02( 8<"( 893-E
-=>$$"8&>( -23( D<9#<( -&"( \-E$0=8^( #02=8-28( ;0&( -EE( 8<"( #-="=( #02=93"&"3( %>( @A""&( "8( -E
\)**)^+
0
0.02
0.04
0.06
0.08
0.1
0.12
012345
α
αα
α
a/h
flood-diminant
ebb-dominaant
(_9/+?+)T(CE8"&2-89:"(A-&-$"8"&='((%-="3(02(8<"("U1-8902
3"=#&9%92/( 8<"( <>A=0$"8&>( 92( 8<"( R"=8"&2( @#<"E38'( 80
#<-&-#8"&9="((8<"("%%[;E003(30$92-2#"(0;(8<"(:"&89#-E(893"
92(8<"("=81-&>+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–27
C=(-E&"-3>(208"3( 92( W<-A8"&(5'(-EE(#-="=(#02=93"&"3(%>(@A""&( "8( -E(\)**)^(#02#"&2(-(;9V"3
E"2/8<(0;(8<"("=81-&>'(8<">(-EE(#02#"&2(=<0&8(-23(A&9=$-89#("=81-&9"='(-23(8<">(-&"(-EE(;&9#8902P
30$92-8"3( #-="=+( J-.92/( 1="( 0;( 8<"( -2-E>="=( 0;( Y9( -23( 6p!022"EE( \)**I^( 02( 893-E
&"#89;9#-8902'(8<"(;0EE0D92/(-3398902-E(A-&-$"8"&=(-&"(93"289;9"3`
!" H<"(&-890(%"8D""2(8<"(E"2/8<(0;(8<"("=81-&>(-23(8<"(D-:"(E"2/8<(0;(8<"(893"+
!" H<"( &-890( %"8D""2( -( E"2/8<P=#-E"( 0;( 8<"( $0&A<0E0/9#-E( :-&9-8902( -E02/( 8<"( "=81-&>
\"+/+(8<"(#<-2/"(0;(D938<^(-23(8<"(D-:"(E"2/8<(0;(893"+
!" H<"(&-890(%"8D""2(8<"(893-E(A"&903(-23(8<"(3"#->(89$"(31"(80(;&9#8902+
_1&8<"&(&"="-&#<(9=(&"U19&"3(80(3"8"&$92"(8<"(&0E"=(0;(8<"="(A-&-$"8"&=+
3.5.4 Tidal asymmetry due to sixth-diurnal tide
@0(;-&(20(8<"0&>(&"E-892/(8<"(893-E(-=>$$"8&>(#-1="3(%>(8<"(=9V8<P391&2-E(893"(<-=(%""2(;0123
92( 8<"( E98"&-81&"+( G;(8<"( =-$"( ;9/1&"( -=( _9/+?+))( ;0&( 8<"(U 1-&8"&P391&2-E( 893"( 9=( $-3"( ;0&( 8<"
=9V8<P391&2-E(893"'(02"(0%8-92=(_9/+?+)I+(C=(8<"(=9V8<P391&2-E(893"( AE->=(-2( 9$A0&8-28(&0E"(92
8<"(R"=8"&2(@#<"E38'(98(9=(&"#0$$"23"3(80(#-&&>(018(&"="-&#<(#02#"&292/(8<"(893-E(-=>$$"8&>
#-1="3(%>(8<9=(/&01A(0;(#02=8981"28='(-23(98=(&"E-8902(D98<(8<"($0&A<0E0/>+
0.9
0.95
1
1.05
1.1
1.15
1.2
1.25
1.3
1970 1975 1980 1985 1990 1995 2000
amplitude parameter
terneuzen/vlissingen
hansweert/terneuzen
bath/hansweert
-25
-20
-15
-10
-5
0
1970 1975 1980 1985 1990 1995 2000
phase parameter
terneuzen-vlissingen
hansweert-terneuzen
bath-hansweert
_9/+?+)I(!":"E0A$"28(0;(8<"(9239#-892/(A-&-$"8"&=(D98<(&"=A"#8(80(8<"(30D2=8&"-$
=8-8902(;0&(JQPJ5
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 3–28
3.5.5 Concluding discussion
CE8<01/<( 8<"( 8<"0&>( ;0123(92( 8<"( E98"&-81&"( 9=( 208( U1-2898-89:"E>( -AAE9#-%E"( 80( 8<"( R"=8"&2
@#<"E38'(8<"(&"=1E8=(A&"="28"3(92(8<"(A&":901=(=1%P="#8902=(#-2(&"-39E>(%"(1="3(80("=89$-8"(8<"
#<-2/"=( 0;( 8<"( 893-E( -=>$$"8&>( 31"( 80( -( #"&8-92( <1$-2( 928"&;"&"2#"( 92( 8<"( "=81-&>'( "+/+( -
;1&8<"&( 3""A"292/( 0;( 8<"( 2-:9/-8902( #<-22"E+( H<9=( #-2( %"( 302"( %>( 3"8"&$9292/( 8<"( 8D0
A-&-$"8"&=(\-[<(-23( ]=[]#^(%";0&"(-23(-;8"&(8<"( 928"&;"&"2#"(-23( AE08(8<"$(92(_9/+?+)5(-23
_9/+?+)?+(H<"(#<-2/"(0;(8<"(E0#-8902=(0;(8<"(A0928=(%";0&"(-23(-;8"&(8<"(928"&;"&"2#"(/9:"=(-2
9239#-8902(0;(8<"(39&"#8902(92(D<9#<(8<"(893-E(-=>$$"8&>(#<-2/"=+(,-="3(02(8<"(-:-9E-%E"(3-8-
98(9=(":"2(A0==9%E"(80(/9:"(-(U1-2898-89:"(A&"39#8902(80(-(#"&8-92("V8"28+
H<9=( D0&.92/( $"8<03( 9=( 92( ;-#8( %-="3( 02( 928"&A0E-8902( [( "V8&-A0E-8902( 1=92/( 8<"( -:-9E-%E"
3-8-+(G8(9$AE9"=(8<"(-==1$A8902(8<-8(8<"(928"&;"&"2#"(D9EE(208(-;;"#8(8<"(-3398902-E(A-&-$"8"&=
$"28902"3(92(?+N+?(92(=1#<(-(D->(8<-8(8<"(&"E-8902(%"8D""2(8<"(893-E(-=>$$"8&>(-23(8<"(8D0
A-&-$"8"&=(1="3(<"&"(D9EE(#<-2/"(=9/29;9#-28E>+
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 4–1
4 Summary, conclusions and
recommendations
H<"( 0%7"#89:"( 0;( 8<"(= 813>( D-=( 80( &":9"D(8< "(8<"0&>( -23( #02#"A8=( 02( 893-E( -=>$$"8&>( -2 3
&"=931-E( ="39$"28( 8&-2=A0&8( 92( "=81-&9"=( -23( 80( -=="=( 8<"9&( -AAE9#-%9E98>( 80( 8<"( R"=8"&2
@#<"E38("=81-&>+(H<9=(#<-A8"&(=1$$-&9="=(8<"(A&92#9A-E(&"=1E8=(-23( #02#E1=902=(0;(8<"(=813>+
,"=93"=( 98( /9:"=( =0$"( &"#0$$"23-8902=( ;0&( ;1&8<"&( &"="-&#<'( 80( ;1&8<"&( 92#&"-="( -23
0A"&-8902-E9="((8<"(.20DE"3/"(-23(123"&=8-2392/(0;(8<"(893-E(-=>$$"8&>'(&"=931-E(8&-2=A0&8=
-23($0&A<0E0/9#(":0E18902(0;(8<"("=81-&>+
H<"(&"=1E8=(0;(8<"(A&"="28(=813>(D"&"(%-="3(02(8<"(;0EE0D92/(-==1$A8902=(-23(&"=8&9#8902=`
!" H<"("=81-&>(9=(D"EEP$9V"3`(<0&9K028-E(-23(:"&89#-E(3"2=98>(/&-39"28=(-&"(2"/E"#8"3+
!" H<"("=81-&>(9=( 893"P30$92-8"3`(8<"(92;E1"2#"( 0;( -( &9:"&( 018;E0D(-23( $"8"0&0E0/9#-E
;0&#92/=(02(8<"(D-8"&($08902(-23(8<"(893-E(-=>$$"8&>(-&"(208(#02=93"&"3+
!" J0=8(0;(8<"(8<"0&"89#-E(-2-E>="=(-23(8<"9&(-AAE9#-8902=(-&"(%-="3(02(-()!(-AA&0-#<+
!" H<"(A"&903(0;(8<"(J5(893-E(#02=8981"28(9=(1="3(-=(8<"(893-E(A"&903+
4.1 Summary and conclusions
C=>$$"8&>( &";"&=( 80( 8<"( "%%P30$92-2#"( 0&( ;E003( 30$92-2#"( 0;( 8<"( :"&89#-E( -23( <0&9K028-E
893"`( 8<"( :"&89#-E( 893"( 9=( ;E003P30$92-28( 9;( 8<"( 31&-8902( 0;( ;-EE92/( 893"( "V#""3=( 8<-8( 0;( 8<"
&9=92/(893"+(O%%P30$92-2#"(0##1&=(92(8<"(0AA0=98"(=981-8902+(H<"(<0&9K028-E(893"(\:"E0#98>^(9=
#02=93"&"3(;E003P30$92-28( 9;( 98( 9231#"=( -( &"=931-E( ="39$"28( 8&-2=A0&8( 92( E-23D-&3( \;E003^
39&"#8902'( D<"&"-=( 98( 9=( "%%P30$92-28( 92( 8<"( #-="( 0;( -( ="-D-&3( 39&"#8"3( &"=931-E( ="39$"28
8&-2=A0&8+(H<"(-=>$$"8&>(0;(8<"(<0&9K028-E(893"($->(%"(-==0#9-8"3(D98<`
!" C2(-=>$$"8&>(92( 8<"( $-/29813"(0;($-V9$1$(;E0D`(;0&(92=8-2#"(9;( $-V9$1$( ;E003
:"E0#989"=( "V#""3( $-V9$1$( "%%( ;E0D( -( ;E003P30$92-28( 8&-2=A0&8( \%"3( E0-3( -23
=1=A"23"3( E0-3^( 9=(E9."E>(80(0##1&'(-=( 8<"( ="39$"28( 8&-2=A0&8( 202PE92"-&E>(92#&"-="=
D98<(8<"(:"E0#98>+
!" C2(-=>$$"8&>(92(8<"(31&-8902(0;(=E-#.(D-8"&`(9;(8<"(31&-8902(0;(=E-#.(D-8"&(%";0&"
;E003(\@,_^("V#""3=(8<"( 31&-8902( 0;( =E-#.(D-8"&( %";0&"( "%%( \@,O^( -2("VA0&8( \"%%P
30$92-2#"^(0;(;92"(=1=A"23"3(="39$"28(9=(;-:01&"3+(R<"2(8<"(A"&903(0;(=E-#.(D-8"&
%";0&"( ;E003( E-=8=( =<0&8"&( 8<"( A"&903( 0;( =E-#.( D-8"&( %";0&"( "%%( -2( 9$A0&8( ( 0;( ;92"
=1=A"23"3(="39$"28(9=(E9."E>(80(0##1&+
H<"(-=8&020$9#-E( 893"( -23(98=(=A-89-EE>(-23(8"$A0&-EE>(:-&>92/(-=>$$"8&>( #-2(%"(3"=#&9%"3
92(8"&$=(0;(-(21$%"&(0;(<-&$029#(#0$A02"28=+(H<"(-$AE9813"(&-890(-23(8<"(A<-="(39;;"&"2#"
0;(J5(-23(98=(0:"&893"=(-&"(0;8"2(1="3(80(#<-&-#8"&9="(8<"(893-E(-=>$$"8&>+
C(8<"0&"89#-E(-2-E>=9=(0;(8<"(9239:931-E(202PE92"-&(8"&$=(92( 8<"()!("U1-8902=(0;($0$"281$
-23( #02892198>( =<0D"3( 8<-8( 0:"&893"=( \JB( "8#+^'( #0$A0123( 893"=( \J@B( "8#+^( -23( 893-E
&"#89;9#-8902( \J0^( -&"( /"2"&-8"3( %>( 8<"( 202PE92"-&( 928"&-#8902=( 0;( 8<"( J5( 893-E( #0$A02"28
D98<(98="E;(\-180P928"&-#8902^(-23(D98<(08<"&(;123-$"28-E(#02=8981"28=`(-(89$"P92:-&9-28($"-2
";;"#8(\&"#89;9#-8902^( -23( 8<"( 0:"&893"( JB( 0&9/92-8"( ;&0$( 8<"( -180P928"&-#8902( 0;( 8<"( J5(:9-
8<&""(202PE92"-&(8"&$='(:9K+`(8<"(-3:"#89:"(92"&89-(8"&$(\,^'(8<"(%0880$(;&9#8902( 8"&$( \!^(-23
Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 4–2
8<"(39=#<-&/"(/&-39"28(8"&$(\F^+(H<"( =9V8<P391&2-E(0:"&893"(-23( #0$A0123( 893"=( \"+/+(JQ('
BJ@Q^( -&"( "=="289-EE>( 31"( 80( 8<"( 202PE92"-&( 928"&-#8902( 0;( J5( D98<( 98="E;( -23( 08<"&
;123-$"28-E(#02=8981"28=(\"+/+(@5^(:9-(8<"(%0880$(;&9#8902(8"&$(\!^+(H<9=($"-2=(;0&(92=8-2#"
8<-8(92(=<-EE0D(893-E(-&"-=(#<-&-#8"&9="3(%>(E-&/"(=A-89-E(:"E0#98>(/&-39"28=(-(/"2"&-8902(0;(JB
9=(E9."E>(80(0##1&(-=(-(&"=1E8(0;(8<"(-180P928"&-#8902(0;(J5(:9-(8<"(%0880$(;&9#8902(8"&$(-23(8<"
-3:"#89:"(92"&89-(8"&$+
M"=931-E(;E0D=($->(=8&02/E>(92;E1"2#"(8<"(-=>$$"8&>(0;(8<"(<0&9K028-E(893"+(H<"9&(/"2"&-8902
9=(:"&>(="2=989:"(80(=A-89-E(:-&9-8902=(92(%-8<>$"8&>(-23(<0&9K028-E(/"0$"8&>'(D<9#<($-."=(98
-(39;;9#1E8(=1%7"#8(80(%"(=8139"3+(H<"(&"=931-E(D-8"&($08902(92(8<"(R"=8"&2(@#<"E38(=""$=(80
%"( 30$92-8"3( %>( %-8<>$"8&>P9231#"3( &"=931-E( ;E0D=`( -8( $-2>( E0#-8902=( 92( 8<"( "=81-&>( 8<"
808-E( #&0==P="#8902-EE>( -:"&-/"3( &"=931-E( #1&&"28( :"E0#98>( 9=( 8<"( 2"8( \=$-EE^( ";;"#8( 0;( -
&"E-89:"E>(E-&/"(&"=931-E(;E003(;E0D(92(8<"(;E003(#<-22"E(-23(-2("%%P30$92-8"3(&"=931-E(;E0D
92(8<"("%%(#<-22"E+(H<"(928"2=98>(\$-/29813"^(0;(&"=931-E(#9&#1E-8902=(9231#"3(%>(8<"("%%(-23
;E003(#<-22"E=(/0"=(8<&01/<(-(2"-AP=A&92/(893-E(#>#E"+
H<"(&"E-8902=<9A(%"8D""2(8<"(-=>$$"8&>(0;(8<"(:"&89#-E(-23(8<"(<0&9K028-E(893"(9=(-(202PE92"-&
02"'( %"#-1="( 8<"( =80&-/"( D938<( -23( #&0==P="#8902-E( -&"-( #<-2/"( D98<( 8<"( D-8"&( E":"E
\<>A=0$"8&>( ";;"#8^+(H<9=(9$AE9"=( 8<-8( -(;E003P30$92-28(31&-8902( -=>$$"8&>( 0;(8<"( :"&89#-E
893"(9=(208(2"#"==-&9E>(-==0#9-8"3(D98<(-(;E003P30$92-2#"(0;(8<"(893-E(#1&&"28+(H<"("E-%0&-8902
0;( 8<9=(&"E-8902=<9A( ;0&( 8<"( R"=8"&2( @#<"E38( =<0D"3( 8<-8(8<"( <>A=0$"8&9#( A&0A"&89"=(0;( 8<"
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 4–3
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4.2 Recommendations
,>( &":9"D92/( 8<"( -:-9E-%E"( .20DE"3/"( 92( 8<"( E98"&-81&"( -23( %>( -2-E>=92/( 8<"( A-&89#1E-&
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 4–4
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 5–1
5 References
C1%&">'(!+F+(n(e+O+(@A""&(\)*IN^(C(=813>(0;(202PE92"-&(893-E(A&0A-/-8902(92(=<-EE0D(92E"8["=81-&92"(=>=8"$='(e-&8
G`(0%="&:-8902='(O=81-&92"'(W0-=8-E(-23(@<"E;(@#9"2#"'(]0E+(5)'(e+)INP5LN+
C1%&">'(!+F+(\)*IQ^'(S>3&03>2-$9#(#028&0E=(02(="39$"28(8&-2=A0&8(92(D"EEP$9V"3(%->=(-23("=81-&9"='(G2(d+(]-2
3"(g&"".(\"3+^(e<>=9#=(0;(=<-EE0D("=81-&9"=(-23(%->='(@A&92/"&P]"&E-/'(,"&E92'(A+(5BNP5NI+
C1%&">'(!+F+(n(W+H+(_&9"3&9#<='(\)*II^'(@"-=02-E(#E9$-80E0/>(0;(893-E(202PE92"-&989"=(92(-(=<-EE0D("=81-&>'(G2(!+F+
C1%&">(n(Y+(R"9=<-&(\"3=+^'(S>3&03>2-$9#=(-23(="39$"28(3>2-$9#=(0;(893-E(92E"8='(@A&92/"&P]"&E-/'
2"D(w0&.'(A+()L?P)5B+
,"&/'(d+S+(:-2(3"2'(J+W+d+Y+(d"1."2(n(C+d+_+(:-2(3"&(@A".(\)**Q^'(S>3&-1E9#(A&0#"=="=(-;;"#892/(8<"($0&A<0E0/>
-23(":0E18902(0;(8<"(R"=8"&=#<"E3"("=81-&>'(92`(U'!1$+"/*&V4-+*'W&U6-%1!"-/<&U/6"+-/)*/!'&$/#&D1)$/
I%!*+/$!"-/''(#<-A8"&(T'("398"3(%>(g+_+(X0&3=8&0$(n(W+H+(M0$-2+
,0/--&3'(Y+C+(198(3"2'()**N+(M"=1E8-8"2(K-23%-E-2=(R"=8"&=#<"E3"()*NNP)**?+(GJCm(&-AA0&8(M(*NPLI'(G2=89818"
;0&(J-&92"(-23(C8$0=A<"&9#(M"="-&#<(m8&"#<8
,002'(d+!+'()*II'(H"$A0&-E(:-&9-8902(0;(=<-EE0DPD-8"&(893"=(92(%-=92P92E"8(=>=8"$='(92(C1%&">(!+F(n(Y+(R"9=<-&
\"3=+^'(S>3&03>2-$9#=(-23(-23(="39$"28(3>2-$9#=(0;(893-E(92E"8='(@A&92/"&P]"&E-/'(X"D(w0&.+
WE-"=="2=(-23(J">:9=(\)**B^+((S"8(0:"&K9#<8(:-2(3"(897D--&2"$92/"2(92(<"8(f""=#<"E3"(%".."2(/"31&"23"(<"8
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 5–2
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics 5–3
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics A – 1
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics A – 2
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics A – 3
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Tidal asymmetry and residual sediment transport in estuaries Z2749 December, 1999
A literature study and applications to the Western Scheldt
WL | delft hydraulics B – 1
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... Residual currents play an important role in net mass transport in the macrotidal estuary (Yanagi et al., 2003). In macrotidal estuaries, it has been known that the residual flow patterns were affected by the increase in nonlinearity process due to overtide (Wang, Jeuken, and De Vriend, 1999) and the vertical and horizontal density structures caused by the increase in freshwater inflow. In addition, since the estuary is continuously affected by artificial influences such as tidal power plants, dams, estuary banks, and submerged structures for human activities, it also leads to changes in residual flow patterns as a result. ...
... On the other hand, the ebb-dominance of the SF was enhanced in both the surface and bottom layers. These increase and decrease in tidal asymmetry also affect the residual flows (Wang, Jeuken, and De Vriend, 1999). The increased vertical salinity gradient near the bridge can enhance the tidal asymmetry (Teng et al., 2022). ...
Conference Paper
Full-text available
Kim, M.H.; Woo, S.-B.; Lee, H.M.; Kim, K.-H.; Song, J.-I., and Kim, J.W., 2023. Impacts of marine construction on tidal and residual characteristics: An example from the Incheon Bridge. In: Lee, J.L.; Lee, H.; Min, B.I.; Chang, J.-I.; Cho, G.T.; Yoon, J.-S., and Lee, J. (eds.), Multidisciplinary Approaches to Coastal and Marine Management. Journal of Coastal Research, Special Issue No. 116, pp. 61-65. Charlotte (North Carolina), ISSN 0749-0208. This study examined the effects on tidal and residual characteristics resulting from the reduction in channel width due to the construction of the Incheon Bridge (IB). Using the three-dimensional numerical model two scenarios were simulated without and with the construction of the IB. Installed piers from the IB construction changed the characteristics of flood and ebb tides, especially near the bridge. As a result, the ebb-dominance on the north side of the navigation channel near the bridge is weakened, and the ebb-dominance on the south side is strengthened. Due to these changes in tidal asymmetry, the residual flow velocity of all vertical layers on the north side of the navigation channel is increased to the ebb direction, strengthening the vertical two-layer circulation. On the other hand, on the south side of the channel, the residual flow velocity of all vertical layers is increased in flood direction, unifying the residual direction of all vertical water columns to the ebb direction. Therefore, the influence of marine constructions such as bridges can play an important role in numerical model studies on tidal and residual characteristics of coastal regions.
... Tidal asymmetry refers to the phenomenon of the tidal wave distortion (Friedrichs and Aubrey, 1988;Wang et al., 1999;Guo et al., 2019), which causes an unequal duration of the rise and fall of tidal height and consequently offsets between the strength of current velocities during flood and ebb tides (Guo et al., 2019). This significantly influences net sediment transport by interacting with the sediment erosion threshold and the settling lags in an estuary (Dyer, 1997;Figueroa et al., 2020a). ...
... The sediments transported by tidal asymmetry are usually balanced with those transported by residual currents (Lin and Kuo, 2001), contributing to the formation of an STM. In general, tidal asymmetry can be classified into tidal duration asymmetry (γ 0 ζ ′ ) and velocity skewness (γ 0 U ) (Wang et al., 1999;Nidzieko and Ralston, 2012). ...
Article
Axial survey and in situ mooring in microtidal Masan Bay were conducted to reveal the mechanism for movement of secondary turbidity maximum (STM) and sediment resuspension. The Bay is characterized by sluggish water circulation with a vertically well-mixed water column. The strength of the residual estuarine current (Δu¯) was enhanced by the combined effects of decreased tidal currents, increased precipitation, and down-estuary (northerly) winds, whereas Δu¯ was weakened by increased tidal currents and up-estuary (southerly) winds. The variability of current asymmetry originated from Δu¯ contributed to the entrapment of suspended sediments, creating a mobile sediment pool in central regions of the Bay. The sediments resuspended from the mobile sediment pool were more influenced by residual currents than the tidal currents, and they remained in suspension near bed. When the down-estuary winds were applied to the mobile sediment pool, the near-bed sediments were readily resuspended to form an STM > 40 mg l⁻¹. The STM moved up-estuary by persistent high Δu¯ and down-estuary by an intermittent low Δu¯. Over the entire measurement periods, the STM moved by at least 450 m toward the up-estuary. As the consolidated sediment layer was exposed by the movement of the STM, near-bed currents were ineffective in resuspending sediments from the consolidated layer even though the winds provided sufficient current strength. Due to the depletion of available sediments for resuspension, the STM was not fully generated. This study highlights that the STM in a microtidal estuary can be determined by the combined function of various forcings such as tide, wind, and precipitation.
... Thus, tide-river interactions can significantly influence tidal duration asymmetry 23 . When tidal elevation and velocity are near quadrature, the tidal duration asymmetry can be related to flow velocity asymmetry 12,30,31 , which has an important influence on sediment transport 17,[32][33][34] . Tidal duration asymmetry also plays an important role in navigation and ecosystems by affecting the fluctuations in water levels and bed friction 22 . ...
... It is common practice to evaluate tidal asymmetry by the harmonics of astronomical tides using the amplitude ratio between the semidiurnal tide M 2 and its first harmonics M 4 (M 4 /M 2 ) to quantify the degree of distortion 15 ; the phase difference (2M 2 − M 4 ) is used as a metric to reflect the direction of tidal asymmetry [12][13][14]32,34,35 . This approach can be extended to evaluate the contributions of triad combinations of tidal constituents, such as K 1 /O 1 / M 2 , which is important in mixed tidal regimes 18,19 . ...
Article
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The Yangtze River Estuary (YRE) is one of the world’s largest river-tidal systems with rapidly changing hydrology and morphology following the construction of multiple dams. The effects of dam construction may extend to the region close to the coast, where channel stability depends on the asymmetry of the tide. Here, we focus on the possible effects of changing discharge regimes on tidal asymmetry in the YRE. Specifically, we focus on the difference in duration between ebb and flood, quantified as tidal duration asymmetry, because it has strong implications for residual sediment transport and can be derived from available water level data. To cope with nonstationary tides under the influence of a time-varying river discharge, a nonstationary harmonic analysis tool (NS_TIDE) is applied to explore the spatiotemporal variations in tidal duration asymmetry, under the influence of different combinations of tidal constituents. Tidal duration asymmetry initially increases, then slightly decreases, in an upstream direction. It experiences significant seasonal variations in response to rapidly varying discharge: tides are more asymmetric upstream of Zhenjiang in the dry season and more asymmetric downstream in the wet season. The combined effects of discharge regulation and morphological changes cause seasonal alterations in tidal duration asymmetry. In the wet season, reduced river discharge caused by water storage and climate change enhance the asymmetry upstream (+11.74% at Wuhu, +7.19 at Nanjing) while the asymmetry is weakened downstream (−2.90% at Zhenjiang, −7.19 at Jiangyin) following the TGD’s operation. Downstream channel erosion caused by post-TGD lower sediment loads has become the dominant factor weakening tidal asymmetry in most parts of the YRE in the dry season. Understanding these evolutions of tidal duration asymmetry under the hydrological and morphological effects has important implications for the management of estuarine ecosystem and navigation.
... Understanding the tidal asymmetrical behavior and variability [9,10,17] and the consequent effects on residual sediment transport and morphodynamics [18][19][20] are helpful in coastal area management [21][22][23]. The difference between durations of rising and falling phases due to tidal asymmetry leads to an offset between the velocities of flood and ebb tides. ...
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The Arvand River forms the border between Iran and Iraq and is the only permanent river discharging into the Persian Gulf (PG). It is a tidal river adversely affected by sedimentation, which is more likely resulted from tidal asymmetry. The tidal barrier (TB) has remarkable effects on the tidal regime of the river. To assess the effects of a tidal barrier on the asymmetry of the tidal waves, it is critical to study the two main factors of closure percentage (CP) and closure duration (CD). This manuscript aims to investigate the tidal barrier effect on the asymmetry of the tidal waves propagating through the estuary. To evaluate tidal asymmetry, a Tidal Asymmetry Index (TAI) is introduced based on the relative phase angle of the M2 and M4 components through the river. A two-dimensional Delft3D hydrodynamic model is utilized. The tidal wave is flood dominant, and its relative phase angle increased slightly, from 90 to 135 degrees in Km 40 and then decreased to just under 90 degrees near the Abadan (65 km) and constant along the Abadan to Khorramshahr. The tidal barrier has changed the tidal regime in the river which leads to relatively constant tidal asymmetry during the 45km upward. To reach the highest TAI in the Arvand estuary, a closure percentage and duration of 55% and 180 minutes are estimated. The tidal barrier operation also adversely affects the amplitude of the M2 and M4 components. M4 component amplitude increases before reaching the TB and then decreases. The decrease is more elaborated from kilometer 45 onward. Increasing the closure percentage amplifies the changes described above, but it has little effect on the general trends.
... The tidal flow (flood or ebb dominance) depends on the relative phase shift from M4 to M2 (Aubrey and Speer, 1985;Yoon and Woo, 2013). Earlier studies associated with tidal asymmetry mainly dealt with long-term datasets from tide gauges or models (Friedrichs and Aubrey, 1988;Guo et al., 2014;Wang et al., 1999) using the stationary harmonic analysis approach. However, a limitation of this method is the high sensitivity to the length of the data set. ...
Article
Understanding tidal dynamics in shallow estuaries is of paramount importance to assess the influence of the parameters control them. In the present study, a comprehensive analysis of the tides in the Wouri estuary (Cameroon) was carried out with a high resolution two-dimensional numerical model. Non-stationary harmonic analysis (S_TIDE) and spatio-temporal variation of tidal asymmetry allowed us to quantify changes and tidal asymmetry metrics in the Wouri estuary. A relative sensitivity coefficient (RSC) was introduced to decompose the contribution of tidal amplitude variations to multiple tidal asymmetries. The result reveal an attenuation of the tidal wave as it propagates inland, with a notable reduction in tidal range. This phenomenon is also amplified by the increase in river flow. The positive values of the asymmetry factor confirm a flood dominance in the upper part of the estuary with a pronounced increase upstream. Conversely, ebb dominance with negative values in the lower part of the estuary. The two tidal combinations M2/M4 and M2/S2/MS4 are identified as the main contributors to the tidal asymmetry in the Wouri estuary. These results allowed the Wouri estuary to be qualified as tidal in its lower part and fluvial in its upper part. The evolution of the tidal amplitude and asymmetry may depend significantly on the variations of the river flow and the morphology of the estuary.
... Tidal flow (flood or ebb dominance) depends on the relative phase shift from M4 to M2 Yoon and Woo, 2013). Previous studies associated with tidal asymmetry have focused on long-term data sets from tide gauges or models (Friedrichs and Aubrey, 1988c;Guo et al., 2014;Wang et al., 1999) using the harmonic analysis approach. However, a limitation of this method is the high sensitivity to the length of the data set. ...
Thesis
L’estuaire du Wouri, situé au coeur du Golfe de Guinée et ouvert sur l’océan Atlantique est soumis à un large éventail d’influence atmosphérique, océanique, continentale et anthropique à différentes échelles de temps (court et long-terme) contrôlant son évolution. La première partie de cette thèse, axée sur des archives remontant au 20ème siècle, a permis de reconstituer l’histoire de l’évolution du littoral estuarien du Wouri. Parallèlement, pour déterminer les tendances d’évolution des hauteurs d’eau, quantifier et qualifier la cinématique du trait de côte et des fonds dans l’estuaire, un travail d’inventaire, de numérisation et d’analyse des documents historiques a été réalisé. Ceci a permis d’enregistrer une évolution du niveau moyen à un rythme d’environ 25mm/an en 17 ans (2002 – 2019). Les résultats ont révélé une prédominance des variations dominées par l’érosion en aval et inversement par l’accrétion en amont, sur la période de 64 ans (1948-2012). Ces tendances sont accentuées par la présence de facteurs amplificateurs (pression anthropique et changement climatique). Afin d’étudier les processus hydrodynamiques et sédimentaires à court terme, une modélisation numérique de la propagation de la marée et la distribution des salinités et des sédiments fins a été réalisée à l’aide de TELEMAC 3D (calibré et validé grâce aux mesures in-situ acquises au cours de l’année 2019). La marée a montré une asymétrie dominée par le jusant dans sa partie inférieure et inversement par le flot dans sa partie supérieure. La distribution de la salinité a permis de caractériser l’estuaire de bien mélangé en vive-eau, particulièrement en étiage à stratifié en morte eau, particulièrement en période de crue. Les variations saisonnières, du régime fluvial ont montré une migration longitudinale de la position de la zone de turbidité maximale : déplacement en amont pendant les étiages et en aval pendant les crues avec pour conséquence une exportation massive de sédiments dans la partie intermédiaire et aval de l’estuaire. Dans un contexte actuel du changement climatique associé aux forts impacts anthropiques, cette étude souligne la nécessité de l’utilisation des archives historiques, de données in-situ couplées à un modèle numérique pour mieux comprendre l’évolution passée et actuelle de l’hydrodynamique et de la dynamique sédimentaire.
... Although our research explores the effects of diverse coastal conditions and accounts for a range of bio-physical processes, model simulations struggle to capture certain profile characteristics, such as the abrupt slope difference between vegetated and unvegetated sections observed in some mangrove environments (e.g., Figures 1a and 1c). The causal factors can be related to different coastal processes and properties, including (a) variations in sediment composition, grain size and mangrove root density across the profile and through depth resulting in differences in sediment erodibility and potentially causing slope differences (Spenceley, 1977;Swales et al., 2007Swales et al., , 2021; (b) complex tidal forcing including overtides of the M2 tidal constituent, such as the M4 and M6 components which modify tidal asymmetry and influence landward sediment transport and thus profile shape (Wang et al., 1999); (c) energetic wave impacts reinforcing mud erosion at the mangrove forest edge (Winterwerp et al., 2013); Figure 11. Relative displacement after 100-year sea-level rise (SLR) impacts. ...
Article
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Mangrove forests are valuable coastal ecosystems that have been shown to persist on muddy intertidal flats through bio‐morphodynamic feedbacks. However, the role of coastal conditions on mangrove behavior remains uncertain. This study conducts numerical experiments to systematically explore the effects of tidal range, small wind waves, sediment supply and coastal slope on mangrove development under sea‐level rise (SLR). Our results show that mangroves in micro‐tidal conditions are more vulnerable because of the gentler coastal equilibrium slope and the limited ability to capture sediment, which leads to substantial mangrove landward displacement even under slow SLR. Macro‐tidal conditions with large sediment supply promote accretion along the profile and platform formation, reducing mangrove vulnerability for slow and medium SLR, but still cause rapid mangrove retreat under fast SLR. Small wind waves promote sediment accretion, and exert an extra bed shear stress that confines the mangrove forest to higher elevations with more favorable inundation regimes, offsetting SLR impacts. These processes also have important implications for the development of new landward habitats under SLR. In particular, our experiments show that landward habitat can be created even with limited sediment supply and thus without complete infilling of the available accommodation space. Nevertheless, new accommodation space may be filled over time with sediment originating from erosion of the lower coastal profile. Consistent with field data, model simulations indicate that sediment accretion within the forest can accelerate under SLR, but the timing and magnitude of accretion depend non‐linearly on coastal conditions and distance from the mangrove seaward edge.
... This is a significant finding because there is a gap in research on understanding the dynamics of tidal flow within drainage ditches. It is known that changing the morphology of a system can affect water movement in the system and potentially change the asymmetry in the tides (Wang et al. 1999), but that this is at a case-by-case basis dependent on the specific water flow alterations (Tonjes 2013). Our results show that the drainage ditch within the Church Flats system fits the expected asymmetry of the South Carolina coast, which is important in determining potential nutrient and pollutant loading (Ellis et al. 2017) and sediment transport of the system (Hoitink et al. 2003). ...
Article
The traditional goal of stormwater management is to reduce the threat of flooding to life and property, and so most landscapes are engineered to maximize the speed at which the unwanted water leaves the watershed. This has been effective in landscapes with some topographic gradient. This often involves the installation of drainage ditches that disperse runoff from urban areas to receiving water bodies; in coastal areas this means a tidal creek, estuary, bay, sounds, or the coastal ocean. This practice reduces flood hazards in some cases but results in unintended effects on the natural hydrology in the watershed and downstream tidal dynamics. For low-gradient watersheds in humid climates, ditch systems also lower the water table of an area, increasing infiltration to recharge and groundwater discharge to streams (baseflow), and larger volume of freshwater delivered downstream yearround. Ditches also create unintentional avenues for the incoming tide from a tidal creek or tidally-influenced waterway to reach further inland, thus reducing the hydraulic gradient between the inland areas and the receiving water body. The combination of these effects can exacerbate compound flooding events, increasing the flood probability if high tide and storm events coincide. Additionally, coastal communities face the challenge of mitigating more complicated flood hazards while land development increases to meet the needs of a growing population. This study analyzed the tidal influence within an inland drainage ditch in the central coast of South Carolina USA that is representative of thousands of artificially-drained coastal watersheds. The ditch-creek system investigated here is 12 km long in a 753-hectare (1860-acre) watershed of Church Flats Creek, a first-order tidal system. We monitored for 13 months a 0.75-km reach of the lower ditch portion of the system, just above the relatively undisturbed tidal creek and marsh. Prior to ditching in the 1960s this system had a wetland-rich floodplain but is now partially tidal. Field data collected were stream stage (depth), discharge, tidal range, tidal volume, incoming (flood) and outgoing (ebb) tidal durations, and water table hydrograph at a location about 50 m of mid-reach of the ditch. Multiple linear regressions were performed to best predict the flood and ebb tidal durations of the system based on tidal characteristics within the ditch. The mean values were 229 ± 2.5 and 182 ± 2.1 minutes for flood and ebb tide durations, respectively and the models explained 84% (residual standard error (RSE) of 25 minutes) and 80% (RSE of 23 minutes) for the flood and ebb conditions, respectively. The models were simulated for sea levels in 1993 and 2050, and results indicate that the flood tide within the drainage ditch is predicted to increase an average of 66 minutes and the total tidal duration (flood and ebb) an average of 139 minutes by 2050. These results suggest a loss in drainage functionality as sea level rises. Increases in the duration of tidal influence will induce a lower capacity for stormwater volume than the drainage infrastructure was constructed to manage, therefore resulting in an increased frequency of compound flooding events because of the lower storage volume and decreased hydraulic gradient in the system. This study fills a knowledge gap of tidal dynamics within coastal ditch-creek systems and we urge stormwater managers to consider the unintended consequences of using traditional stormwater methods in a region that does not benefit from gravity drainage practices like in other regions.
... In macro-tidal estuaries, hydrodynamics is mainly governed by tides which, have a profound impact on residual sediment dynamics and consequently on morphological evolution (Zhang et al., 2018). As examined by several authors Speer and Aubrey, 1985;Friedrichs and Aubrey, 1988;Nidzieko and Ralston, 2012;Guo et al., 2018), tidal asymmetry plays an important role, causing residual sediment transport in estuarine systems (Wang et al., 1999;McLachlan et al., 2020;Mandal et al., 2020), and can be computed from flow velocity and water elevation (Friedrichs and Aubrey, 1988;Nidzieko and Ralston, 2012;Bolle et al., 2010). The former identifies the nature of the asymmetry: i.e., ebb-or flood-dominance in the estuary. ...
Article
The Rance estuary is a relatively small low-discharge, steep-sided ria, located along the Brittany coast in northern France, with a maximum spring tidal range of 13.5 m. Taking advantage of this hyper-tidal regime, the first and currently the second largest operational tidal power station in the world was built at the estuary's mouth and has been in operation since the 1960s. Despite the well-known effect of damping of estuarine water levels, little attention has been given to quantifying the influence of the plant on the propagation and asymmetry of the tidal wave inside the estuary. In this study, hydrodynamics and tidal wave patterns were analyzed in this anthropogenically influenced estuarine system. A two-dimensional depth-averaged numerical model of the Rance estuary was developed. Two scenarios without the tidal power plant involving the dam's pre- and post-construction bathymetry (1957 and 2018 respectively) and present-day conditions scenarios were designed, to highlight the impact of bed evolution and the tidal power station on hydrodynamics and tidal asymmetry. Numerical results showed that, without the structure, bathymetric evolution did not substantially influence estuarine hydrodynamics. Nevertheless, on the estuary-side of the dam, the presence of the tidal power plant induced (i) a decrease in both tidal range and tidal prism, (ii) an increase of low water levels, and (iii) a decrease in both flood and ebb currents. Contrastingly, the region close to the structure reacted differently to plant operating modes, with an increase in flood currents (ebb currents) upstream of the sluice gates (downstream of the turbines). For both the natural condition and the artificially-induced hydrodynamic forcing due to the presence of the plant, numerical results showed that the Rance estuary mainly exhibits flood-dominant behavior, with a longer duration of falling than rising water and stronger peak flood currents than ebb currents. Spanning a period of approximately 60 years, this study presents a quantitative analysis of the influence of the tidal power station on the hydrodynamics in the Rance estuary, and its possible consequences for sediment dynamics. This approach is novel for this particular enclosed water body, characterized by the presence of a dam at its mouth and a lock at its uppermost limit.
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