RI Coastal Resources Management Council
...to preserve, protect, develop, and restore coastal resources for all Rhode Islanders
...to preserve, protect, develop, and restore coastal resources for all Rhode Islanders
Illustrates and displays storm inundation, with and without sea level rise, for different types of storms that could occur along Rhode Island’s coast line.
The Coastal Resources Management Program (CRMP) has developed regulations for reconstruction after "the big one" as well as other severe storms (Section 180. Emergency Assents). More important are the regulations that are designed to minimize the impact of coastal hazards. Policies regulating where to build on a vulnerable property (Section 140. Setbacks), construction of shoreline protection facilities (various sections), and beneficial reuse of dredged materials help to mitigate some of the hazards associated with coastal living. Sea level rise is a hazard that is only indirectly addressed in the CRMP. Erosion setbacks are very effective regulations that protect the homeowner and the public resources. Much of the Rhode Island shoreline is eroding. Erosion rates are calculated by comparing the shoreline location from historic aerial photographs to the most recent shoreline position. Sections of the south shore barriers have erosion rates of more than three feet per year. That is an average rate over time. In reality, the shoreline may erode tens of feet in a single storm, followed by some accretion. In critical erosion areas on barriers, all residential construction with less than six units must be set back 30 times and commercial property 60 times the average annual erosion rate. The farther the house or commercial structure is setback from the shore, the longer it will last. Unfortunately, these regulations were enacted about thirty years ago. The Council may want to consider policy for when the setback is gone and the structure is on the active beach (figure 1).
Figure 1. House pilings in the wave swash. Old pilings and ISDS exposed after a storm.
Impacts of storm erosion on ISDS are a potential public health problem (figure 2). CRMC worked with RIDEM to develop regulations for repairs to ISDS in critical erosion areas (ISDS Repair Guidance in Critical Erosion Areas, January 31, 2006).
Figure 2. ISDS exposed by storm surge and waves.
Shoreline Protection Structures are prohibited along Type 1 shorelines except where they are used to protect historic structures that are listed on the National Register of Historic Places (Section 220). There are several reasons for this prohibition. The structures reflect wave energy, often causing erosion around the sides of the structure and can cause scouring seaward of the structure. In addition, the structures disrupt sediment transport, both by sequestering sediment that would normally erode from a bank or dune to form new beaches (figure 3), and by physically blocking the sand movement along the shoreline (figure 4). Shoreline protection structures often impact lateral public access along the shoreline. In other words, these structures help protect the property where they are built, but often harm adjacent properties. They are a contributing factor in the narrowing and loss of beaches, and they inhibit the public's right to lateral shoreline access (figure 5). Many of the structures that were built prior to the CRMP cannot withstand moderate storms (figure 6).
Figure 3. Sediment that erodes from the headland bluffs forms the beaches. The dotted line marks the extent of the slump block before the sediment was transported by waves and currents.
Figure 4. The jetty interrupts the longshore sand transport.
Figure 5. Lateral access is limited to low tide.
Figure 6. Many shoreline protection structures cannot withstand moderate storm energy.
CRMC advocates the beneficial reuse of dredged material. The South Coast Habitat Restoration Project is an example of beneficial reuse that has created wider beaches and has the secondary benefit of providing protection for some coastal properties (figure 7).
Figure 7. Beach with dredged sand on the left shows no erosional scarp. The beach on the right shows dune scarp and newly exposed ISDS.
NOAA's updated outlook for the 2024 Atlantic Hurricane Season indicates that an above-normal season is most likely, with low possibilities the season could be near-normal and even lower odds for a below-normal season. The outlook calls for an 85% chance of an above-normal season, along with a 10% chance for a near-normal season and a 5% chance for a below-normal season. See NOAA definitions of above-, near-, and below-normal seasons. The Atlantic hurricane region includes the North Atlantic Ocean, Caribbean Sea, and Gulf of Mexico.
The updated 2024 outlook calls for a 70% probability for each of the following ranges of activity during the 2024 hurricane season, which officially runs from June 1st through November 30th:
2024 Objectives
Extended Range Forecast of Atlantic Seasonal Hurricane Activity and Landfall Strike Probability for 2024 (PDF) from CSU Tropical Weather and Climate Research
"We have slightly increased our forecast and continue to call for an extremely active Atlantic hurricane season in 2024. Sea surface temperatures averaged across the hurricane Main Development Region of the tropical Atlantic and Caribbean remain near record warm levels. Extremely warm sea surface temperatures provide a much more conducive dynamic and thermodynamic environment for hurricane formation and intensification. We anticipate cool neutral ENSO or La Niña during the peak of the Atlantic hurricane season, resulting in reduced levels of tropical Atlantic vertical wind shear. Hurricane Beryl, a deep tropical Category 5 hurricane, is also a likely harbinger of a hyperactive season. This forecast is of above-normal confidence. We anticipate a well above-average probability for major hurricane landfalls along the continental United States coastline and in the Caribbean. As with all hurricane seasons, coastal residents are reminded that it only takes one hurricane making landfall to make it an active season. Thorough preparations should be made every season, regardless of predicted activity."
Probabilities of tropical storm-force, hurricane-force and major hurricane-force winds occurring at specific locations along the U.S. East and Gulf Coasts within a variety of time periods are listed on the Landfall Probability Web site. The site provides U.S. landfall probabilities for 11 regions and the individual counties along the U.S. coastline from Brownsville, Texas, to Eastport, Maine. Individual state probabilities are also available. The website, available to the public at http://hurricanepredictor.com, is the first publicly accessible Internet tool that adjusts landfall probabilities for regions and counties based on the current climate and its projected effects on the upcoming hurricane season.
RI Emergency Management Agency:
National Hurricane Center Resources
Hurricanes: Science and Society – Major goals of Hurricanes: Science and Society are to provide foundational science for understanding complex scientific content, inform visitors about current scientific and technological advances, and to help visitors make good decisions prior to and during a hurricane emergency.
The following lists the relevant sections of the Coastal Resources Management Plan dealing with coastal hazards.
Post Storm Actions:
Section 1.1.14 Emergency Assents
Pre Storm Mitigation:
Section 1.1.9 Setbacks
Section 1.2.2(A) Coastal Beaches
Section 1.2.2(B) Barrier Islands and Spits
Section 1.2.2(D) Coastal Headlands, Bluffs and Cliffs
Section 1.2.2(G) Dunes
Section 1.3.1(G) Construction of Shoreline Protection Facilities.
Section 1.3.1(I) Dredging and Dredged Materials Disposal
Stedman Government Center
Suite 116, 4808 Tower Hill Road, Wakefield, RI 02879-1900
Voice 401-783-3370 • Fax 401-783-2069 • E-Mail cstaff1@crmc.ri.gov
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