Living Shorelines in Connecticut |
Why Living Shorelines The Connecticut Coast Types of Living Shorelines Design Considerations Permitting Resources Printer Friendly Version |
Beaches and Dune
Beaches and dunes are dynamic
features affected by short and long term changes in waves, wind, tides, storm
surge, sand availability and sea level rise. These
changes may be seasonal, episodic or storm-related, or slow, barely noticeable
change over many years. Beach and dune erosion along the Connecticut shoreline of Long Island Sound is generally
caused: |
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SEASONAL CHANGES |
Seasonal storms and variations in local wind speed and direction can cause
short-term changes in the beach profile. Summer beaches tend to be wider than
their corresponding winter beach, with a well-developed berm. Winter beaches
are steeper and narrower. These changes are minimized along Connecticut
beaches due to the buffering effect of ocean winds and the limited fetch
caused by Long Island. |
STORMS |
Storm impacts occur over a very
short period but recovery of the beach may occur with seasonal changes or
over a much longer period of time. In the case of severe storms, recovery of
the beach may not occur at all. |
SAND
AVAILABILITY |
Sand availability can change when sand is moved offshore during storms
and is no longer available for beaches, or when sand transported landward
during storms is removed as debris. |
MANMADE
STRUCTURES |
Groins, seawalls and jetties can exacerbate coastal erosion by
interrupting the natural transport of sediment. |
CURRENTS |
Alongshore
and cross-shore currents can transport sediment away from beaches,
contributing to shoreline erosion. |
PUBLIC ACCESS |
Foot traffic can damage the dune
vegetation reducing dune stability against wave and winds. |
CLIMATE
CHANGE |
The Connecticut shoreline has
been affecting for decades by rising sea levels. Sea level rise may adversely
affect beaches that are not able to migrate landward over time. |
Several options are available for addressing beach and dune
erosion; 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. Is there a sand
dune at the seaward edge of the property? If so, is it vegetated? If not, is a
dry beach present (sand above normal high tide)? If yes, how wide?
An existing dune
indicates the suitability and viability of dune restoration at the project
site. The presence of vegetation on the dune not only provides an indication of
the stability of the dune system, but is important when creating a dune
restoration and planting plan.
If the beach is not
currently backed by a dune, there needs to be sufficient dry beach width to
create a dune system. In some areas, beach nourishment may be permitting which
could extend the width of the beach to allow dune creation.
3. Is there evidence
that your dune or backshore is regularly overtopped and overwashed by waves,
and/or that flooding occurs landward of the dune or beach crest? During normal
or spring tides? Storm surges?
The frequency of
dune or backshore overtopping and flooding is important when determining the
necessary elevation of coastal protection to mitigate coastal inundation.
4. Does the dune and beach naturally gain sand after each winter season?
Beach and dune
systems change in response to seasonal variations in waves, wind, tides, and
storm surge, transforming from a. wider, flatter “summer” beach to a narrower,
steeper “winter” profile. Because the Connecticut shoreline is protected from
ocean winds by Long Island, the seasonal variation in winds is less pronounced
than on more exposed shorelines. It is important to consider seasonal
variations in beach profile when selecting and designing a Living Shoreline.
5. Is the beach eroding?
If so, what is the rate of erosion and what is causing it?
Do nothing or dune vegetation
management may be suitable approaches for a stable beach/dune system 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.
6. 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.
7. 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.
8. 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.
9. 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.
10. 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.
11. 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 beach. Steep nearshore
bathymetry will allow larger waves to break on the beach. Larger winter waves
or storm waves typically transport available sand offshore, forming protective
sand bars.
12. 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.
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. How will the
shoreline be used?
The intended use of
the shoreline may affect the suitable types of living shoreline. For instance,
swimming and boating require different access to the water than fishing or
nature watching. The selected type of living shoreline must be compatible with
the intended usage of the shoreline.
17. 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, traditional, hard
coastal protection structures may limit the effectiveness of a living
shoreline.
18. Is the project site
accessible from land or water?
Access to the
project site will affect the cost and constructability of a living shoreline.
19. 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 beach
and dune systems are not eroding include:
For beaches with low waves and limited boat traffic, gradual
nearshore and insufficient land to create a dune system:
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Jennifer O'Donnell, Ph.D.
Coastal Ocean Analystics, LLC
860.961.2467
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