…………………. support many wavelike motions
The governing equations
waves are broadly defined as
oscillations of the dependent variables
Some of the waves supported by the equations are:
Some of these waves are important for the
dynamics of synoptic scale systems
Some of these waves are important for the dynamics of synoptic scale systems, while others are merely
noise
In order to understand dynamic meteorology, we must understand
the waves that can occur in the atmosphere.
what are the governing equations?
set of equations that controls processes in the atmosphere
ex: momentum
what does a wave mean? (particles)
particles are not moving (stationary)
what is the difference between oscillations and waves?
oscillations
sin and cosine can be applied to both
whenever you see sin and cosine think of
waves
define amplitude
half of the difference in height between a crest and a trough
define wavelength
(,) – the distance between crests (or troughs)
define wavenumber
K= 2pi/lamda
the number of radians in a unit distance in the direction of wave propagation. (sometimes the wave number is just defined as 1/lamda, in which case it is the number of wavelengths per unit distance.)
A higher wave number means
a shorter wavelength.
units of wavenumber
Units are radians m-1, or sometimes written as just m-1
We can also define wave numbers along each of the axes.
The wave number vector is given by

define angular frequency
(w) 2 pi times the number of crests passing a point in a unit of time.
angular frequency units
radians s-1, sometimes just written as s-1.
define phase speed
(c) the speed of an individual crest or trough.
phase speed for a wave traveling solely in the x-direction
c = w/k.
phase speed for a wave traveling solely in the y-direction
c = w/l.
phase speed for a wave traveling solely in the z-direction
c = w /m
phase speed for wave traveling in an arbitrary direction
c = w /K, where K is the
total wave number given by K2= k2+ l2+ m2