Abstract
This paper considers the flow over a mountain which has elliptical contours, for two types of undisturbed air stream. In the first case the static stability parameter
l
2
=
gB
/V
2
is assumed to be constant throughout the atmosphere, and in the second
l
2
is assumed to fall off exponentially with height, in each case with (
V’’/V
) =
q
2
also being constant. On the basis of the wave equation derived in an earlier paper, a simpler method is developed to find approximations to the difficult Fourier integrals which arise. The results show that when
l
2
is constant the form of the waves is determined by the value of q. When
q
= 0 the waves lie in a strip in the lee of the highest part of the mountain, but when
q
is large enough the waves are contained in a wedge, and resemble ship waves. When
l
2
falls off exponentially the waves closely resemble ship waves for any value of
q
. The variation of the amplitude of the waves as various parameters are changed is discussed in detail.
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