Hydraulics Prof. B.S.
Thandaveswara
37.3 Classification of waves
Translatory, longitudinal shallow water waves can be classified based on different
criteria as shown in table below. (Ref. unsteady flow in open channels edited by
Mahmood K and Yevjevich V. Vol 1, 1975).
Table: Criteria for classification of wave
Criteria Classification
Surges (Moving hydraulic jugs - hydraulic bore)
(1) Rate of
variation Intermediate waves
Long waves
capillary wave
gl
Gravity C 2 =
2π
(2) Controlling
force
(
gL 2πσ
)
2πy
C2 = ___ + ____ tanh ____ (for shallow water waves)
2π ρL ρL
Capillary wave
(
gL 2πσ
C2 = ___ + ____
2π ρL ) (for deep wave)
Gravity and friction
3a
η = 2a S ec h 2 ( x − ct )
Simple solitary 2 y3
(Single form of gravity wave )
Undisturbed water flow
a
η
(3) Frequency of
occurrence
The Solitary Wave
Indian Institute of Technology Madras
Hydraulics Prof. B.S. Thandaveswara
Mutiple
Wave train
cg
Wave Groups
Downstream
Relative to channel bed slope
Upstream
Vw Vw Vw
y V2 V2 y V2 y V2 y
2 V1 y1 y1 V1 2 y1 V1 2 y V1 2
1
Type A - Advancing Type B - Advancing Type B - Advancing Type B - Advancing
downstream upstream upstream upstream
(positive surge) (positive surge) (positive surge) (positive surge)
Vw = c + V1 Vw = c - V1 Vw = c + V1 Vw = c - V1
(4) Direction of
movement
V - Vw+V2 Vw - V2 +V
y w V2 Vw - V1 V +V y Vw - V1 y y Vw 2 Vw+V1
2 y1 y w 1 2 y1 2 2 y1
1
Type A Type B Type C Type D
Four Types of rapidly varied uniformly progressive flow. (Top)
Unsteady flows; (bottom) the corresponding flows that appear steady to
an observer following the wavefront.
Downstream
Relative to underlying flow
Upstream
(5) Wave
surface
elevation
Indian Institute of Technology Madras
Hydraulics Prof. B.S. Thandaveswara
Positive(higher) uniformly
progressive wave (sluice gate)
Relative to level of underlying flow Surge
Negative(lower) Type C (Sluice gate)
and D is operated Demand Surge
Positive-negative (when Sluice is operated these these appear in pairs)
Occur Tidal in rivers
Type A, B occur in Tidal rivers
Rejected Surge
(6) Form Single-faced (Monoclinical progressive rising wave)
Symmetrical
Two-faced
Asymmetrical
FLOOD
WAVE
Q
Time
Mean Water Level L
η a
(7) Periodic or
oscillatory wave
A Periodic y
Definition Sketch for Oscillatory Wave Motion
Particles constantly progressing the wave movement (Example: Sea waves)
(8) Translatory
Orbital
Circular particle Orbits in Deep Water
Indian Institute of Technology Madras
Hydraulics Prof. B.S. Thandaveswara
(9) Transverse
wave
Longitudinal
wave
L
Mean water level
(10) Deep water
wave
Stokesian wave
Cnoidal wave y
Shallow water y'
wave
Elliptical Particle Orbits in Shallow Water
Mean water level
Typical Cnoidal Wave Profile
(11) Mechanical
Oscillation Finite amplitude due to initial disturbance
(pulsating flows) Mechanical oscillation
Kinematic wave Surface instability
Eg: Roll wave (progressive wave train)
Diffusive wave Steep slopes F > 2.0
Dynamic wave
(12)Rapidly
varying Progressing Surges, bores, depression
unsteady flow
Gradually Floods in reservoirs and in channels / rivers
varying
unsteady flow
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