Open Access. Powered by Scholars. Published by Universities.®
![Digital Commons Network](http://assets.bepress.com/20200205/img/dcn/DCsunburst.png)
Physical Sciences and Mathematics Commons™
Open Access. Powered by Scholars. Published by Universities.®
Articles 1 - 7 of 7
Full-Text Articles in Physical Sciences and Mathematics
Anthropocene Sea Level Change: A History Of Recent Trends Observed In The U.S. East, Gulf, And West Coast Regions, John D. Boon, Molly Mitchell, Jon Derek Loftis, David L. Malmquist
Anthropocene Sea Level Change: A History Of Recent Trends Observed In The U.S. East, Gulf, And West Coast Regions, John D. Boon, Molly Mitchell, Jon Derek Loftis, David L. Malmquist
Reports
Relative sea level (RSL) observations since 1969 at U.S. tide stations exhibit trends in RSL rise rate and acceleration that vary in response to both global and regional processes. Trend histories display a high degree of similarity between locations in coastal regions that are experiencing similar processes. With the exception of the U.S. Northeast Coast and Alaska,every other coastal location in the continental U.S. has experienced an upturn in RSL rise rate since 2013-2014 despite wide differences in the magnitude and trending direction of RSL acceleration. High RSL acceleration along the U.S. Northeast Coast has trended downward since 2011 while …
Shoreline Evolution: City Of Chesapeake, Virginia Elizabeth River Shorelines Data Summary Report, Donna A. Milligan, Christine Wilcox, C. Scott Hardaway Jr.
Shoreline Evolution: City Of Chesapeake, Virginia Elizabeth River Shorelines Data Summary Report, Donna A. Milligan, Christine Wilcox, C. Scott Hardaway Jr.
Reports
City of Chesapeake is situated between the Cities of Norfolk and Portsmouth along several branches of the Elizabeth River (Figure 1). Because the City's shoreline is continually changing, determining where the shoreline was in the past, how far and how fast it is moving, and what factors drive shoreline change will help define where the shoreline will be going in the future. These rates and patterns of shore change along Chesapeake Bay’s estuarine shores will differ through time as winds, waves, tides and currents shape and modify coastlines by eroding, transporting and depositing sediments.
The purpose of this report is …
Monitoring Of Suspended Sediment Plume Formed During Oyster Shell Dredging In The James River, Virginia, August 2001, Carl T. Friedrichs, Grace M. Massey
Monitoring Of Suspended Sediment Plume Formed During Oyster Shell Dredging In The James River, Virginia, August 2001, Carl T. Friedrichs, Grace M. Massey
Reports
No abstract provided.
Shoreline Management Plan With Habitat Enhancement For Town Of Saxis, Virginia, C. Scott Hardaway Jr., Donna A. Milligan, George R. Thomas, Rebecca C.H. Brindley, Lyle M. Varnell, Walter L. Priest, Sharon Dewing
Shoreline Management Plan With Habitat Enhancement For Town Of Saxis, Virginia, C. Scott Hardaway Jr., Donna A. Milligan, George R. Thomas, Rebecca C.H. Brindley, Lyle M. Varnell, Walter L. Priest, Sharon Dewing
Reports
The goal of the present study is to identify the best course of action to manage shoreline erosion in Saxis and to provide a detailed Shoreline Management Plan with Habitat Enhancement which can be presented to potential State and Federal funding agencies. While the Plan itself will not resolve the erosion conditions in Saxis, it will allow the Town to market its need and the method of resolution of this need, to agencies and leaders with the resources to implement the Plan’s suggested actions. The shoreline management plan will provide the necessary level of shoreline stabilization while minimizing adverse impacts …
Water Quality Conditions In The Tidal Rappahannock River: Longitudinal And Dome Surveys In 1993, Kyeong Park, Albert Y. Kuo
Water Quality Conditions In The Tidal Rappahannock River: Longitudinal And Dome Surveys In 1993, Kyeong Park, Albert Y. Kuo
Reports
Previous field surveys and modeling studies (Kuo et al. 1991; Park et al. 1993) indicated the presence of three different water quality regimes in the tidal Rappahannock River (Fig. 1), a western shore tributary of Chesapeake Bay: : Region I - hypoxic conditions during summer in the bottom water between km 0-55 : Region II - high chlorophyll concentration between km 80-147 : Region III - waste water discharges from sewage treatment plants To study the differences among these 3 reaches of the river, two types of field surveys were conducted during the summer of 1993: 1) longitudinal surveys in …
Ware River Intensive Watershed Study - Part 2. Estuarine Receiving Water Quality, Cindy Bosco, Gary F. Anderson, Bruce Neilson
Ware River Intensive Watershed Study - Part 2. Estuarine Receiving Water Quality, Cindy Bosco, Gary F. Anderson, Bruce Neilson
Reports
The Ware River Intensive Watershed Study contains results of runoff from small catchments, instream transport of runoff and the impacts on estuarine water quality, which are contained in two volumes: 1. Nonpoint Source Pollution and 2. Estuarine Receiving Water Quality
Estuarine Studies: The Ware River is a relatively "clean" estuarine system. However, during summer months some of the nutrients, particularly inorganic phosphorous and organic nitrogen, achieve levels associated with moderate enrichment. The Ware is typical of other small tributaries of Chesapeake Bay: nutrient levels are higher at low tide, the estuary is more homogenous laterally than longitudinally, and vertical gradients …
Ware River Intensive Watershed Study- Part 1. Nonpoint Source Contributions, Gary F. Anderson, Cindy Bosco, Bruce Neilson
Ware River Intensive Watershed Study- Part 1. Nonpoint Source Contributions, Gary F. Anderson, Cindy Bosco, Bruce Neilson
Reports
Runoff quantity and quality were monitored for row crop, residential and forested lands in the Ware basin for the period of October 1979 to July 1981. Loading rates have been calculated for both baseflow and stormflow contributions at each study site.