Living Shorelines in Connecticut |
Why Living Shorelines The Connecticut Coast Types of Living Shorelines Design Considerations Permitting Resources Printer Friendly Version |
MarshesMarshes occur in sheltered areas with low to moderate wave energy; however, they still may be experience erosion caused by:
For more information on the design parameters, click here. Several options are available for addressing erosion of
coastal marshes; the most appropriate method will depend on site specific
conditions. There are many parameters to consider before selecting a Living
Shoreline approach. Some questions to
ask are: 1.
Is there an
existing coastal engineering structure (seawall, groin, revetment, etc.) at the
site? The presence of an
existing engineering structure may affect the coastal processes at the site and
must be considered before an appropriate living shoreline approach can be
determined. If the structure is functioning as designed, or easily repaired,
the most appropriate approach may be to do nothing or repair the structure,
while considering alternatives for future needs. See Currently
Defended Shorelines for more information on coastal
engineering structures. 2. What is the
condition of the marsh? Is there presently a vegetated wetland at the edge of
the property? Is the vegetation dense or sparse? How wide is the marsh? The condition of the existing
marsh is an indication of the potential success of a living shoreline approach.
A marsh with dense, healthy vegetation is likely to be a suitable site for a
non-structural approach. A less dense marsh may be enhanced with vegetation
management, trimming or overhanding branches and removal of fallen trees and
debris. 3. Is the marsh
eroding? If so, what is the rate of erosion and what is causing it? Do nothing or
vegetation management may be suitable approaches for a stable marsh with little
to no erosion. With higher rates of erosion, it is necessary to determine what
is causing the erosion. Mitigating erosion from frequent boat
wakes
may indicate a different approach than one used to reduce storm
flooding
and wave damage. While seasonal damage may not be a cause for concern, a marsh
may take years to recover from significant ice damage. 4. Is there
infrastructure at risk? If the existing
infrastructure cannot be moved back or up, it may be necessary to select an
approach that would provide more protection than a non-structural approach. Evaluation
of the site may determine that a living shoreline approach is unsuitable. 5. What is the wave
climate? The wave climate is
a critical parameter in determining the most appropriate approach to shoreline
protection. Vegetation-only approaches are usually only suitable for site
exposed to low wave heights. The wave climate will determine the type of living
shoreline, and the height and composition of the protective structure. Fetch, the
distance wind blows of water, is frequently used as an estimate of the wave
conditions at a site. 6. What is the boat
traffic? Some sites, particularly
those along navigable rivers streams, may experience larger waves due to boat
wake than wind waves. The proximity to a powerboat marina or navigational
channel, and the frequency and size of vessels are an important design
consideration. 7. Is the site
affected by tidal, riverine or alongshore currents? Nearshore currents
can scour protective structures and transport fill material away from the
project site. 8. What is the
shoreline geometry? The Connecticut shoreline
of Long Island Sound is highly variable. The shoreline geometry may be
straight, curved or irregular. This high variability is one reason why the most
suitable approach to shoreline protection is so site-specific. A headland beach
(also known as a pocket beach) is generally crescent or crenulate-shaped,
bounded by protective headlands so the shoreline is relatively protected and
the sediment supply usually remains between the headlands. A straight shoreline
is more exposed to large waves and transport of sediment away from the site. 9. What is the
intertidal slope/nearshore bathymetry? The intertidal
slope and nearshore bathymetry determine the size of the waves at the
shoreline. A gradually sloping nearshore region will cause larger waves to
break further offshore, reducing the wave energy at the marsh. Steep nearshore
bathymetry will allow larger waves to break near or at the marsh edge. 10. Is the upland bank
vegetated? Upland vegetation
is an indication of the stability of the bank. However, mature vegetation may
provide too much shade for marsh plant survivability. 11. What is the tidal
range? The tidal range
will impact the height and location of the shoreline protection approach. Most
of the existing living shoreline structures have been constructed in areas with
low tidal ranges on the order of a couple of feet. Tidal ranges along the
Connecticut shoreline vary from about 2.4 ft in Stonington to 7.5 ft in Greenwich.
In addition, storm surge heights are typically larger in Connecticut than where
living shorelines have been constructed previously. 12. Does the project
site flood regularly during normal or spring tides? Storm surge? Flooding of coastal
marshes is a natural process; however, if the site floods during normal or
spring tides, the marsh may not provide sufficient protection from storm waves.
Marshes typically do not provide protection from storm surge, so the potential
risk from coastal inundation is an important design consideration. 13. Is the project site
affected by ice? The Connecticut
coast is affected by ice damage, exacerbated by nor-easters and tidal flow. The
approach selected must withstand anticipated ice forces at the site. 14. Does the site have
submerged aquatic vegetation or nearshore oyster beds? Submerged aquatic
vegetation or the presence of nearshore recreational oyster beds may affect the
type of living shoreline that can be permitted at the site. 15. What is the
composition of the nearshore region? Some soils may not
be able to tolerate the weight of living shoreline approaches such as marsh
sills
or reef balls. Settling of the
structure could render it ineffective. The presence of offshore vegetation or
aquatic species may be negatively impacted by the living shoreline. For
instance, fill material could bury aquatic
plants and animals, or sills and breakwaters could damage
nearshore habitats. 16. What is the
condition of the adjacent properties? Depending on the
width of the project site, the condition of adjacent properties may affect the
suitability of living shoreline approaches. For instance, the presence of marsh
may indicate the suitability of the site for marsh creation or restoration.
Hard coastal structures may limit the effectiveness of a living shoreline. 17. Is the project site
accessible from land or water? Access to the
project site will affect the cost and constructability of a living shoreline. 18. What are the
potential effects of sea level rise on the project site? Depending on the
anticipated lifetime of the living shoreline, the effects of sea level rise on
the erosion mitigation approach may be a selection factor. A printable checklist of design considerations can be found here. Some of the options for mitigating coastal erosion on
marshes are: For marshes that are not eroding: For marshes experiencing erosion,
options to consider include:
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Jennifer O'Donnell, Ph.D.
Coastal Ocean Analystics, LLC
860.961.2467
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