Physical Sciences and Mathematics Commons^™

Cruise: Yr080610, Stations: S4636- S4650, Clay Bank, York River Virginia 3-Hour Mudbed Calibration Survey Bracketing A Slack To Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 3-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr080729, Stations: S4651- S4776, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr090108, Stations: S4730- S4757, Gloucester Point, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr090226, Stations: S4758- S4781, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr090514, Stations: S4802- S4819, Clay Bank, York River Virginia ~4-Hour Mudbed Calibration Survey From Max Ebb To Max Flood, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a ~4-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location

Cruise: Yr110901, Stations: S4976- S4995, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr120430, Stations: S4998- S5014, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr120724, Stations: S5026- S5040, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr130206, Stations: S5084- S5096, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr130521, Stations: S5100- S5124, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr130912, Stations: S5208- S5236, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr111220, Stations: S4989- S5004, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velocimeter (ADV) tripod deployed in nearby location.

Cruise: Yr121006, Stations: S5038-­S5077, Clay Bank, York River Virginia 6-­Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.||During each station in the survey a profile or bottom time series was collected with a suite of instrumentation including: a RDI 1200 KHz ADCP, a YSI 6600 CTD, a Sequia LISST 100X, a Sontek ADVOcean and a PICS floc camera. The raw Data of profile stations is processed to provide a smooth profile of Data throughout the water column and a series of between 2 …

Cruise: Yr110818, Stations: S4947- S4967, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr091125, Stations: S4847- S4872, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing An Ebb Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Cruise: Yr110816, Stations: S4941- S4946, Clay Bank, York River Virginia 1.5-Hour Mudbed Calibration Survey, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 1.5-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location. The survey was aborted early due to rough weather

Cruise: Yr090811, Stations: S4820- S4846, Clay Bank, York River Virginia 6-Hour Mudbed Calibration Survey Bracketing A Flood Tide, Grace M. Cartwright, Carl T. Friedrichs

Data

Dataset consists of profile and water column burst Data and bottom burst Data collected as part of a 6-hour anchor station survey in support of an Acoustic Doppler Velicometer (ADV) tripod deployed in nearby location.

Designing Improved Sediment Transport Visualizations, Chris Englert, Thomas J. Butkiewicz, Larry A. Mayer, Val E. Schmidt, Jonathan Beaudoin, Arthur Trembanis, Carter Duval

Center for Coastal and Ocean Mapping

Monitoring, or more commonly, modeling of sediment transport in the coastal environment is a critical task with relevance to coastline stability, beach erosion, tracking environmental contaminants, and safety of navigation. Increased intensity and regularity of storms such as Superstorm Sandy heighten the importance of our understanding of sediment transport processes. A weakness of current modeling capabilities is the ability to easily visualize the result in an intuitive manner. Many of the available visualization software packages display only a single variable at once, usually as a two-dimensional, plan-view cross-section. With such limited display capabilities, sophisticated 3D models are undermined in both …

Interpretation Of Biological Activity Using An Acoustic Backscatter Sensor (Abs), Courtney Elliton

Honors Theses

Acoustics aid in the description of complex processes, such as the suspension of sand particles exposed to local hydrodynamic forces above a rippled bed (Cacchione, et al., 2008). Acoustic data can be applied to several aspects of the marine environment such as marine chemistry, biology, geology, and ecology. The acoustic data collected in this study was part of a larger, grant-funded project that focused on sediment transport and settlement preference on two offshore hardbottoms following beach renourishment along the heavily developed coast in northeastern South Carolina. Acoustic data collection was used in the larger project to describe changes in sediment …

Algal Biomass Accrual In Relation To Nutrient Availability Along A Longitudinal Gradient In The Upper Green River, Kentucky, Mary Douglas Penick

Masters Theses & Specialist Projects

Nutrient limitation in aquatic ecosystems results from a deficiency in nitrogen or phosphorus levels relative to cellular growth needs. Nutrient limitation of freshwater systems is a function of biotic and abiotic factors. Biotic factors include vascular and nonvascular plant community composition. Abiotic factors include underlying bedrock and land-use activities (e.g. agriculture, septic systems). Nutrient availability directly affects growth, productivity, and community structure of primary producers. The purpose of this study was two-fold: (1) to assess the relationship between ambient algal biomass. and in-stream nutrient levels along the longitudinal course of a river through a transition from weak to well-developed underlying …

Geological Analysis And Hydrodynamic Modeling Of Tropical Cyclone Influence: Northeastern Gulf Of Mexico Inner Shelf, Amy Lynn Spaziani

LSU Master's Theses

The need to characterize offshore resources as borrow areas for beach restoration has initiated interest of the impact of storms to the inner continental shelf. While numerous studies have investigated the response of coastal systems to major storms, very little is known about the geological response of inner shelves to frequent and intense storms. This approach integrated a geological study with modeling of hydrodynamics during recent storms, in order to relate trends in the geological signature to physical forcing mechanisms during storms. First, waves and hydrodynamic conditions were modeled during two major recent storms that made landfall in the northeastern …

Arctic Perennial Ice Cover Over The Last 14 Million Years, Dennis A. Darby

OES Faculty Publications

Knowledge of the long-term history of the perennial ice is an important issue that has eluded study because the Cenozoic core material needed has been unavailable until the recent Arctic Coring Expedition (ACEX). Detrital Fe oxide mineral grains analyzed by microprobe from the last 14 Ma (164 m) of the ACEX composite core on the Lomonosov Ridge were matched to circum-Arctic sources with the same mineral and 12-element composition. These precise source determinations and estimates of drift rates were used to determine that these sand grains could not be rafted to the ACEX core site in less than a year. …

Sources Of Sediment Found In Sea Ice From The Western Arctic Ocean, New Insights Into Processes Of Entrainment And Drift Patterns, Dennis A. Darby

OES Faculty Publications

The geochemical fingerprint of entrained Fe oxide mineral grains in Arctic Ocean sea ice is used to determine precise sources of this sediment. This approach substantiates the importance of the Laptev Sea as a source of sea ice and even the presence of Russian ice in the Beaufort Sea off Alaska. Fe oxide grains from the Laptev Sea were found in floes in the Beaufort Sea, Chukchi Borderland, and central Arctic Ocean, demonstrating the importance of sea ice in distributing itself throughout the Arctic Ocean and the potential of transporting sediment from Russian rivers to North American shelves. Banks Island …

Cross-Shoreface Suspended Sediment Transport : A Response To The Interaction Of Nearshore And Shelf Processes, Fall 1994 Duck, Nc Field Experiment, D. A. Hepworth, Carl T. Friedrichs, John Brubaker

Reports

Deployment : The tripods were assembled, tested and secured onboard the RIV Sea Diver, which left the Little Creek Amphibious Base in Norfolk, Virginia early on 26 September. While underway to the deployment site, the continuous surface water conductivity and temperature survey was run and several CTD casts were made. The tripods were deployed on 26 September and secured to the sea floor with sand anchors by VIMS divers. The R/V Sea Diver then began the series of on/off shore transects at the tripod deployment site for approximately 12 hours. The vessel returned to port on 27 September .

Recovery: …

Sediment Budgets And Shoreline Dynamics Cape Henry, Virginia, Marcia R. Berman

OES Theses and Dissertations

Analysis of 1183 beach profiles from Cape Henry, Virginia indicated that the recession-erosion ''rule" established by the Army Corps of Engineers underestimates the short-term response of the shoreline to changes in sediment volume.

Correlation between bi-weekly backshore volume change and the change in high water line (HWL) position was stronger (0.67 < r < 0.88) than correlation between bi-weekly total volume change and the change in mean low water (MLW) shoreline position (0.33 < r < 0.52). The short-term change in position of MLW is influenced by minor features such as bars. The position of the HWL is controlled by volume change at the backshore.

Correlation between change in HWL and MLW shoreline positions improved from r = 0.01 tor·= 0.67 for intervals of two weeks to two years, respectively. This suggests parallel-shore retreat only may be operable for greater than two-year periods.

Cross-Shore Sediment Transport In Relation To Waves And Currents In A Groin Compartment, Hyo Jin Kang

OES Theses and Dissertations

In nearshore areas waves are generally irregular, and the irregular wave-induced currents have different peak velocities (magnitude asymmetry) and durations (duration asymmetry) between forward and backward motions. These asymmetries may produce a net cross-shore sediment transport in one direction. The sediment transport mostly occurs as bedload where the waves are non-breaking.

Sediment transport on a sloping bed is also affected by gravity, and accordingly the Shields parameter should be re-evaluated for a grain on a sloping bed. It was also found that the affect of a steady current that interacts nonlinearly with the waves was important for the cross-shore sediment …

Characteristics Of Sediment Transport In Overwash Surges, Paul Richardson Bowen

OES Theses and Dissertations

Sediment samples taken from a washover deposit were used to determine the mode of sediment transport within overwash surges. The determination of sediment transport mode is based on the concept of hydraulic equivalency of different density grains. Hydraulic equivalency may be based on settling velocities or entrainment velocities. Two individual mineral grains of different densities cannot have the same settling and entrainment velocities. If the settling velocities of each grain are similar, then the less dense grain must be physically larger to settle at the same rate as the smaller denser mineral. However, once both of these grains have made …