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Transient Long-Wave Response for a Multiple-Island System
Transient Long-Wave Response Multiple-Island System
2009/4/2
An interpretation of the tsunami response at the Hawaiian island of Kauai has been carried out utilizing simple geometric representations which include the three-island system of Kauai, Niihau and Oah...
On Long-Wave Disturbances of Dynamic Height in the North Pacific
Dynamic Height On Long-Wave Disturbances North Pacific
2009/3/7
Long-wave disturbances of dynamic height in the North pacific are investigated by means of closely spaced STD (salinity, temperature, depth) stations and are related to atmospheric forcing. Wavelike d...
Long waves are affected by bottom topography and under certain conditions may be trapped along topographical contours which then act as wave guides transmitting wave energy for great distances with li...
It is shown that resonant coupling between ultra long equatorial Rossby waves and packets of either short Rossby or short westward-traveling gravity waves is possible. Simple analytic formulas give th...
Evaluation of Frictional, Wind-Forced Long-Wave Theory on the West Florida Shelf
Frictional West Florida Shelf Wind-Forced Long-Wave Theory
2009/1/12
Clarke and Van Gorder have recently formulated a model describing the large-scale, low-frequency response of continental shelf waters to synoptic-scale wind stress in terms of a sum of forced waves. T...
Interannual Westward-Propagating Baroclinic Long-Wave Activity on Line P in the Eastern Midlatitude North Pacific
Baroclinic Long-Wave Interannual Westward-Propagating
2009/1/7
For the period 1959–81, quasi-zonal hydrographic sections have been made between the southern coast of Vancouver Island (49°N, 126°W) and Ocean Station P (50°N, 145°W) approximately every two months. ...
Long-Wave Generation Due to the Refraction of Short-Wave Groups over a Shear Current
Long-Wave Generation Shear Current Short-Wave Groups
2008/12/27
The generation of long waves by short-wave groups propagating over a shear current is studied. The incident wave groups consist of two co-linear short waves with slightly different frequencies. These ...