Tidal analysis of the Barren Island restoration area

doi:10.25923/xtfd-mc44

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Tidal analysis of the Barren Island restoration area

2022
By Center for Operational Oceanographic Products and Services (U.S.)
Series: NOAA technical report NOS CO-OPS ; 099

[PDF-2.86 MB]

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Corporate Authors:

Center for Operational Oceanographic Products and Services (U.S.)
NOAA Program & Office:

NOS (National Ocean Service) ; CO-OPS (Center for Operational Oceanographic Products & Services)

NOS (National Ocean Service) ; CO-OPS (Center for Operational Oceanographic Products & Services) Less -
Description:

Barren Island is one of many islands in the Chesapeake Bay that have diminished in size due to sea level rise and erosion (Figure 1) (Kearney, M.S. and J.C. Stevenson, 1991). Over the past several hundred years, erosion and overwash episodes induced by storm surge formed several small connections from the main body of the estuary into what is now known as the Honga River (Wray, 1995). These small tributary connections slowly grew under tidal forcing and currents and created an island chain that reached longitudinally from the central Chesapeake Bay region to the south.
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Barren Island Inundation The Center For Operational Oceanographic Products And Services (CO-OPS) Tidal Analysis
Series:

NOAA technical report NOS CO-OPS ; 099
DOI:

https://doi.org/10.25923/xtfd-mc44
Document Type:

Technical Report
Rights Information:

Public Domain
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Submitted
Main Document Checksum:

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urn:sha256:f68513eb0558f8df91354dd599d451d3ca3dac3504c915b3574f1548a142d991
Download URL:

https://repository.library.noaa.gov/view/noaa/47713/noaa_47713_DS1.pdf
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Tidal analysis of the Barren Island restoration area

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