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The Virginia Wetlands Report Vol. 11, No. 3, Virginia Institute Of Marine Science Oct 1996

The Virginia Wetlands Report Vol. 11, No. 3, Virginia Institute Of Marine Science

Virginia Wetlands Reports

  • Great Blue Heron. Julie G. Bradshaw
  • Weakfish. Lyle Varnell
  • Geographic Information Systems Support Tributary Strategy Planning in Virginia. Marcia Berman
  • Wetlands and Regional Watershed Management. Katie Hopkins
  • Cranberries. Pam Mason
  • What is a groin and how does it work? William Roberts


The Virginia Wetlands Report Vol. 11, No. 2, Virginia Institute Of Marine Science Mar 1996

The Virginia Wetlands Report Vol. 11, No. 2, Virginia Institute Of Marine Science

Virginia Wetlands Reports

  • Northern Harrier, or Marsh Hawk. Julie G. Bradshaw
  • Bay Anchovy. Lyle Varnell
  • Geographic Information System (GIS) Data Exchange- The State of the Problem, Part 2. Marcia Berman
  • General Assembly Passes, and Governor Signs Wetlands Mitigation Banking Legislation.
  • Second Edition of the Virginia Wetlands Management Handbook Now Available.
  • Wetlands Management Symposium: Wetlands Compensation Survey Results
  • Westmoreland State Park. Pam Mason
  • Literally, what is littoral sand movement? William Roberts


Effects Of Channel Geometry On Cross Sectional Variation In Along Channel Velocity In Partially Stratified Estuaries, Carl T. Friedrichs, John M. Hamrick Jan 1996

Effects Of Channel Geometry On Cross Sectional Variation In Along Channel Velocity In Partially Stratified Estuaries, Carl T. Friedrichs, John M. Hamrick

VIMS Books and Book Chapters

Analytic solutions for along‐channel velocity through an estuarine cross‐section with laterally varying depth are compared to observations from an array of current meters deployed over a nearly triangular cross‐section of the James River estuary. Analytic results suggest that the transverse structure of along‐channel velocity at this cross‐section is primarily due to simple density‐driven circulation modified by bathymetry. Comparisons of analytic solutions for the amplitude and phase of tidal velocity to observations suggest that linear models which include realistic lateral depth variation should also incorporate across‐channel variation in eddy viscosity. Solutions for various contributions to mean velocity are then derived which …


The Virginia Wetlands Report Vol. 11, No. 1, Virginia Institute Of Marine Science Jan 1996

The Virginia Wetlands Report Vol. 11, No. 1, Virginia Institute Of Marine Science

Virginia Wetlands Reports

  • Black Skimmer. Julie G. Bradshaw
  • Alewife. Lyle Varnell
  • Geographic Information System (GIS) Data Exchange- The State of the Problem. Marcia Berman
  • Northern Neck Workshops Prove Profitable to Participants. Beth Peacock
  • Grazing and Haying Activities in Wetlands. Pamela Mason
  • Should I fertilize my tidal marsh? William Roberts


Introduction, Carl T. Friedrichs, D. G. Aubrey Jan 1996

Introduction, Carl T. Friedrichs, D. G. Aubrey

VIMS Books and Book Chapters

No abstract provided.


Uniform Bottom Shear Stress And Equilibrium Hyposometry Of Intertidal Flats, Carl T. Friedrichs Jan 1996

Uniform Bottom Shear Stress And Equilibrium Hyposometry Of Intertidal Flats, Carl T. Friedrichs

VIMS Books and Book Chapters

Hypsometry is the distribution of horizontal surface area with respect to elevation. Recent observations of tidal flat morphology have correlated convex hypsometry with large tide ranges, long‐term accretion and/or low wave activity. Concave hypsometry, in turn, has been correlated with small tide ranges, long‐term erosion and/or high wave activity. The present study demonstrates that this empirical variation in tidal flat hypsometry is consistent with a simple morphodynamic model which assumes tidal flats to be at equilibrium if maximum bottom shear stress (τ) is spatially uniform. Two general cases are considered: (i) dominance of τ by tidal currents, where τ is …