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Dune erosion models and swash zone kinematics from remote video observations

Creator:: Palmsten, Margaret L.
Abstract:: The subaerial beach, composed of sand dunes and the foreshore, provides a natural buffer zone between vulnerable land and the dissipation of storm wave energy due to wave breaking. The natural beauty of this region is attractive to people, and as a result, significant investment has been placed in this...
Resource Type:: Dissertation
Full Text:: : _____________________________________________________________________ Robert A. Holman The subaerial beach, composed of sand dunes and the foreshore, provides a

Development of 2D models to estimate nearshore bathymetry and sediment transport

Creator:: Splinter, Kristen D.
Abstract:: We examine the interactions and feedbacks between bathymetry, waves, currents, and sediment transport. The ﬁrst two pro jects focus on the use of remote sensing techniques to expand our knowledge of the nearshore. Due to the plethora of snap-shot data that is available from satellites and their distribution via Google...
Resource Type:: Dissertation
Full Text:: - posed by Lippmann and Holman (1990). . . . . . . . . . . . . . . . . . . . 2 2.1 Example of a linear

Standing edge waves on a pocket beach

Creator:: Culley, Sara K.
Resource Type:: Masters Thesis
Full Text:: ). The greatest thanks to my major professor and boss, Dr. Rob Holman, a very clever fellow who taught

Edge waves in the presence of strong longshore currents

Creator:: Howd, Peter A.
Resource Type:: Dissertation
Full Text:: ' Oceanography presented on May 6. 1991 Robert A. Holman The wave-induced velocity field in the nearshore is

Shoreline rhythmicity on a natural beach

Creator:: Garrow, Holly C.
Resource Type:: Masters Thesis
Full Text:: by R-mode factor analysis on a data set in which each contour is normalized to the same mean and

Edge wave response to a modulating incident wave field

Creator:: Lippmann, Thomas Charles
Resource Type:: Dissertation
Full Text:: chapters will be co- authored by R. A. Holman. Chapter 4 will appear later this year in the Journal of

Beach foreshore response to long-period waves in the swash-zone

Creator:: Howd, Peter A.
Abstract:: A field experiment designed to test the hypothesis that infragravity and lower frequency waves influence the patterns of erosion and deposition on the beach foreshore has been carried out. The data show coherent fluctuations in the foreshore sediment level which can be related to low frequency wave motions. The fluctuations...
Resource Type:: Masters Thesis
Full Text:: south. -4. -3. G -2 R A H SI z 2 3. 4. E L E (M)X I 0 N 5- MSL 5- ' I'\ \ - _''s'I

Statistical distribution of swash maxima on natural beaches

Creator:: Holland, K. Todd
Abstract:: Beach response to overwash processes is a topic of significant importance. Two particular aspects of this topic were chosen for detailed analysis: the distribution of maximum wave runup elevations and the cross-beach celerity gradient of overwash bores on natural beaches. Data were collected using both traditional nearshore instrumentation and recently...
Resource Type:: Masters Thesis
Full Text:: significant infragravity energy, commonly a dominant component of field runup signals (Holman, 1981), for

The sediment response of a dissipative beach to variations in wave climate

Creator:: Haxel, Joseph H.
Abstract:: Using wave and wind data from nearby buoys and gauges, real time kinematic global positioning system (RTK-GPS) and light detection and ranging (lidar) topographic survey data, and a robust video record, we have quantified the Large Scale Coastal Behavior (LSCB) of a dissipative end member beach in the Pacific Northwest....
Resource Type:: Masters Thesis
Full Text:: Dissipative Beach toVariations in Wave Climate. Abstract Approved: Robert A. Holman Using wave and wind

Remote measurements of waves and currents over complex bathymetry

Creator:: Chickadel, Carmine C. (Carmine Christopher)
Abstract:: Waves are the primary input of energy in the nearshore region, and together with the currents forced through the transfer of momentum that occurs during the wave breaking process they are the principal mechanism for sediment transport in the nearshore. The basic physics of waves and currents are thought to...
Resource Type:: Dissertation
Full Text:: : ___________________________________________________ Robert A. Holman Waves are the primary input of energy in the nearshore region, and

ScholarsArchive@OSU

Dune erosion models and swash zone kinematics from remote video observations

Development of 2D models to estimate nearshore bathymetry and sediment transport

Standing edge waves on a pocket beach

Edge waves in the presence of strong longshore currents

Shoreline rhythmicity on a natural beach

Edge wave response to a modulating incident wave field

Beach foreshore response to long-period waves in the swash-zone

Statistical distribution of swash maxima on natural beaches

The sediment response of a dissipative beach to variations in wave climate

Remote measurements of waves and currents over complex bathymetry

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