 |
|
New York Ratings
 |
 |
 |
 |
 |
 |
 |
 |
Indicator Type |
 |
Info |
 |
Status |
 |
 |
 |
 |
 |
Beach Access |
 |
6
|
 |
4 |
 |
 |
 |
 |
 |
Water Quality |
 |
6
|
 |
4 |
 |
 |
 |
 |
 |
Beach Erosion |
 |
6 |
 |
- |
 |
 |
 |
 |
 |
Erosion Response |
 |
- |
 |
5 |
 |
 |
 |
 |
 |
Beach Fill |
 |
5 |
 |
- |
 |
 |
 |
 |
 |
Shoreline Structures |
 |
5 |
 |
4 |
 |
 |
 |
 |
 |
Beach Ecology |
 |
6
|
 |
- |
 |
 |
 |
 |
 |
Surfing Areas |
 |
2 |
 |
7
|
 |
 |
 |
 |
 |
Website |
 |
5 |
 |
- |
 |
 |
 |
 |


|
New York Beach Erosion
Erosion Data
Approximately 47% of New York's shoreline is critically eroding, according
to the report "State Coastal Program Effectiveness in Protecting Natural
Beaches, Dunes, Bluffs, and Rock Shores" (T. Bernd-Cohen and M. Gordon),
Coastal Management 27:187-217. 1999.
The average coastal erosion rate along the south shore of Long Island, NY has been calculated at 1-2 ft/year. This erosion rate is relatively small compared to most of the rest of the East Coast. The beaches along the south shore of Long Island are relatively stable but tend to experience significant erosion during major coastal storms. Although not well understood by the general public, breaches, washovers and inlet migration are natural processes that help accumulate sand for natural protective features such as dunes, beaches and marshes. Prevention of these processes could lead to long term instability of the coastal barriers.
According to the Division of Coastal Resources Web site, ongoing coastal erosion and flooding present
complex problems that must be addressed by coastal residents, coastal users,
and all levels of government in the state. The Office of Coastal, Local Government and Community Sustainability (Office)
is undertaking actions which are intended to correct past mistakes and improve
decision-making. These include implementation of sand bypassing at inlets
to restore the natural system of shore protection, erosion monitoring to
enrich the coastal processes database for making informed coastal management
decisions, and technical assistance to all levels of government to ensure
best management practices in addressing site-specific problems.
A cooperative program has been established by NYSDOS with the US Army Corps
of Engineers, New York Sea Grant, and local governments to monitor coastal
erosion on barrier islands and beaches along the south shore of New York
City and Long Island. The New York Sea Grant Web site provides
a nice summary of erosion issues and New York's collaborative monitoring
effort in the Winter 2000 issue of its Coastlines publication.
Erosion data for the south shore of Long Island are kept by NYSDOS, the U.S.
Army Corps of Engineers, and New York Sea Grant. Erosion data were last updated
in Spring 2003. Erosion information on the entire New York coast is kept
by the Department of Environmental Conservation (DEC). Coastal Erosion Hazard
Area maps are available for the coast of New York from the DEC.
New York has identified areas of high erosion rates ("Structural Hazard Areas"),
which they define as having long-term erosion rates greater than one foot
per year. These areas are mapped (see above paragraph), but the maps are not available online.19
Long Island's coast is a dynamic environment, constantly changing in response
to natural processes and human activities. The 125 miles of ocean coast stretching
across its densely populated south shore from Coney Island to Montauk is
of particular interest due to the high level of development in this area.
For example, Long Beach is a barrier island with a year round population
of 50,000. "Coastal erosion along the south shore is a significant problem
for all levels of government," says NYSG coastal processes and facilities
specialist Jay Tanski. "Historical maps and aerial photos show that the patterns
of shoreline change are highly variable in this area. Some areas appear to
be stable or even gaining sand over the last century while others are eroding
at tens of feet per year." The key to sound coastal management is having
a good understanding of how the shoreline is behaving and what is causing
these changes. "In addition to natural processes such as storms and sea level
rise," Tanski says, "human activities - primarily those associated with stabilizing
and dredging the inlets for navigation purposes - have impacted the patterns
and rates of erosion in the area."
An article Coastal Bluff Recession and Impacts on Littoral Transport: Special Reference to Montauk, NY by Frank S. Buonaiuto Jr. and Henry Bokuniewicz was published in the Fall 2005 issue of Shore & Beach, a publication of the American Shore & Beach Preservation Association. Data analysis indicates that bluff recession for the Montauk reach delivered approximately 34,480 cubic meters of sediment to the shoreline per year during the six-year study period, containing an estimated 21,720 cubic meters of beach-suitable sand. Volumetric bluff recession rates varied from 1.0 m3/m/yr to 19.6 m3/m/yr. The study noted that "Bluffs can be stabilized through various combinations of slope reduction, controlled drainage, vegetation, and engineered structures, however this will reduce the volume of material supplied to the littoral system."
In recent years, Long Island's south shore has been impacted by a number
of major storms that have resulted in serious flooding and erosion in many
communities. Estimates of the value of public and private structures and
property in these south shore areas prone to erosion and flood are upwards
of $10 billion.
Working with Dr. Henry Bokuniewicz, a researcher at the State University
of New York (SUNY) at Stony Brook's Marine Sciences Research Center (MSRC)
and DeWitt Davies of Suffolk County Planning, Tanski developed a model monitoring
program based on the experiences of similar programs across the country and
input from local officials. This resulting monitoring program, specifically
designed to provide managers, planners and their coastal users with information
they could use to make better decisions regarding erosion management along
the south shore, incorporates six different elements. They include periodic
aerial photography of the shoreline, measurements of the condition of the
beach twice a year and measurements of the waves causing shoreline changes.
Using the information and materials from Sea Grant's efforts, the NYSDOS
Division of Coastal Resources worked with the U.S. Army Corps of Engineers
New York District to begin implementing the program. With the support of
both federal and state legislators, a $1.4 million annual appropriation to
fund the Atlantic Coast of New York Monitoring Program (ACNYMP) was included
in the Federal Water Resources Development Act.
The monitoring program, which was administered by the Planning Division of
the Corps New York District, is a cooperative effort with overall program
guidance and direction provided by a "study team." This group comprises representatives
from the Corps, the NYSDOS Office of Coastal, Local Government and Community Sustainability, the NY Department
of Environmental Conservation and New York Sea Grant.
Although lapses in the funding stream have prevented full implementation
of the program, a considerable amount of data has been collected from some
348 locations along the shore. In addition to taking measurements of beach
volume and elevation, aerial photographs of the entire shoreline have been
taken twice a year since 1995. State supplemental funds are used by the NYSDOS
to address additional data gathering needs. "We want to be sure that we are
getting all the data needed by local governments and regulators to facilitate
wise management of our coastal resources," says Fred Anders of the State's
Office of Coastal, Local Government and Community Sustainability.
Each of the cooperating agencies in the program serves as a repository
for data products, enhancing dissemination of the information generated by
ACNYMP to the widest range of audiences: local governments, regulatory agencies,
scientists, engineers, and other interested parties. New York has more recently developed a coastal analysis package in partnership with the State University of New York at Stony Brook. Principal authors of that package are Dr. Henry Bokuniewicz and Dr. Brian Batten. The package can be viewed within the Atlantic Coast of New York Monitoring Program Web site by clicking on the "View Data" link.20
The Long Island Regional Planning Board prepared a report, Proposed Long
Island South Shore Hazard Management Program that contains shoreline change
information for Fire Island to Montauk. The Atlantic Coast of New York Erosion
Monitoring Program plans to update the data in this report, which is now
20 years old but still useful for long-term trends. In addition, topographic
maps and orthophotos of the entire state, including all the coastal areas,
can be viewed and downloaded at http://www.nysgis.state.ny.us.21
Erosion rates on the open ocean beaches of New York can range from 0 to 7
feet per year. Beaches along the south shore are susceptible to long-term
erosion, but the eastern end of Fire Island and other sites down-drift of
inlet jetties, have experienced significant erosion. Other than this, little
detailed information appears to be readily available.
In the winter of 2005-2006, beaches and dunes on the South Shore of Long Island and bluffs on the island's north shore sustained significant erosion for early "nor'easter" storms in October 2005.
General information on coastal processes and erosion, particularly for New York's Great Lakes shoreline, can be found at:
http://www.cce.cornell.edu/seagrant/erosion/erosionpages/erosionpubs.htm
The Heinz Center's Evaluation of Erosion Hazards, conducted for the Federal
Emergency Management Agency, studied the causes of coastal erosion hazards
and proposed a variety of national and regional responses. The study, published
in April 2000, concentrates on the economic impacts of erosion response policies
and the cost of erosion itself to homeowners, businesses, and governmental
entities. The study notes that average shoreline positions in parts of Long
Island have fluctuated over the past 160 years but overall have receded approximately
350 feet. The report states that average erosion rates are 1-2 ft/year in Suffolk, NY.
A NOAA Web site that has graphs of sea level data for many coastal locations around the country over the last 40 to 50 years and projections into the future is http://tidesandcurrents.noaa.gov/sltrends/sltrends.shtml
NOAA recently launched the NOAA Shoreline Web site. The site is a comprehensive guide to
national shoreline data and terms and is the first site to allow vector
shoreline data from NOAA and other federal agencies to be conveniently
accessed and compared in one place. Supporting context is also included
via frequently asked questions, common uses of shoreline data, shoreline
terms, and references. Many NOAA branches and offices have a stake in
developing shoreline data, but this is the first-ever NOAA Web site to
provide access to all NOAA shorelines, plus data from other federal
agencies. The site is a culmination of efforts of NOAA and several
offices within NOS (including NOAA’s Coastal Services Center, National
Geodetic Survey, Office of Coast Survey, Special Projects Office, and
Office of Ocean and Coastal Resource Management) and other federal
agencies to provide coastal resource managers with accurate and useful
shoreline data. For more information, contact Tara Miller (tara.miller@noaa.gov).
Erosion Contact Info
Barry Pendergrass
New York State Department of State
Office of Coastal, Local Government and Community Sustainability
99 Washington Avenue
Albany, NY 12231
Phone: (518) 486-3277
Email: Barry.Pendergrass@dos.state.ny.us
Hazard Avoidance Policies/Erosion Response
See Erosion Response section.
|