The response of a basin with a topographic barrier to spatially localized a
nd time periodic forcing is considered. The barrier, which almost completel
y divides the full basin into two adjacent subbasins, is offered as a model
of either a planetary island in the wind-driven circulation or a portion o
f the midocean ridge in the abyssal circulation.
The barrier completely blocks the flow between the two adjacent subbasins e
xcept for the possibility of flow through two small gaps at the termini of
the barrier. The barrier has nonzero thickness, and scale-dependent Lateral
friction acts in the gap channels to impede the flow from one subbasin to
the next. Bottom friction also acts uniformly on the flow in the basin. The
degree to which localized forcing is able to excite large-scale motions in
the adjacent subbasin is shown to be connected to the structure of the for
cing and its frequency.
In the absence of forcing and friction a set of full basin normal modes exi
st. The degree to which the forcing is able to resonate with such modes det
ermines the degree to which energy can be transmitted from one subbasin to
the other. Friction in the gaps reduces both the amplitude of that transmis
sion and smooths the peaks of the response curve of the motion as a functio
n of frequency in both subbasins. However, even for substantial friction, a
considerable amount of large-scale variability can be excited in the adjac
ent basin. The quantitative dependence of the response on the degree of fri
ction, the length of the channels representing the gaps, and the meridional
structure of the forcing are discussed.
In cases where the western boundary of the basin is nonreflecting, so that
no full basin normal modes are possible, substantial energy transmission is
still demonstrated. Whether resonance occurs or not, the necessity for ene
rgy transmission is closely related to the existence of the integral circul
ation constraint around the island barrier and the possibility of resonance
acts mainly to set the level of the response.