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Full-Text Articles in Oceanography and Atmospheric Sciences and Meteorology

Strokes For Representing Univariate Vector Field Maps, David Fowler, Colin Ware Jun 1989

Strokes For Representing Univariate Vector Field Maps, David Fowler, Colin Ware

Center for Coastal and Ocean Mapping

Particle systems make an excellent tool for creating tracks (which we call strokes) in vector fields. The question addressed in this paper is how such tracks should be made to vary in size and colour in order to reveal properties such as local direction and strength of the field. We find that for strokes that vary from large to small, direction is indicated by the large end. We also find that for strokes that vary in colour, the colour of the background is the most important determinant of perceived direction.


Escim: A System For The Investigation Of Meaningful Motion, Siew Hong Yang, Colin Ware Jun 1989

Escim: A System For The Investigation Of Meaningful Motion, Siew Hong Yang, Colin Ware

Center for Coastal and Ocean Mapping

A language is described whose purpose is the investigation of meaningful motion using Stimulus Response animation techniques. The language is capable of adjusting the shape, size and velocity of an actor in real-time computer animation. Some results are presented showing how it is possible to generate such behaviours as chasing, avoidance and hitting using this animation technique. A set of primitives are presented which we find invaluable in the control of size, stretch and velocity parameters when attempting to produce fluid and meaningful interactions.


Sea Beam Survey Of An Active Strike-Slip Fault: The San Clemente Fault In The California Continental Borderland, Mark R. Legg, Bruce P. Luyendyk, Jacqueline Mammerickx, Christian De Moustier, Robert C. Tyce Feb 1989

Sea Beam Survey Of An Active Strike-Slip Fault: The San Clemente Fault In The California Continental Borderland, Mark R. Legg, Bruce P. Luyendyk, Jacqueline Mammerickx, Christian De Moustier, Robert C. Tyce

Center for Coastal and Ocean Mapping

The San Clemente fault, located in the California Continental Borderland, is an active, northwest trending, right-lateral, wrench fault. Sea Beam data are used to map the major tectonic landforms associated with active submarine faulting in detail unavailable using conventional echo-sounding or seismic reflection data. In the area between North San Clemente Basin and Fortymile Bank, the major late Cenozoic faults are delineated by alignments of numerous tectonic landforms, including scarps, linear trenches, benches, and sags. Character and spatial patterns of these landforms are consistent with dextral wrench faulting, although vertical offsets may be substantial locally. The main trace of the …