New York Harbor Storm-Surge Barrier

Last updated

Map of proposed storm surge storm surge barrier system for New York Harbor. New York Regional Barrier System.jpg
Map of proposed storm surge storm surge barrier system for New York Harbor.

The New York Harbor Storm-Surge Barrier is a proposed flood barrier system to protect the New York-New Jersey Harbor Estuary from storm surges. The proposed system would consist of one barrier located across the mouth of Lower New York Bay, possibly between Sandy Hook (N.J.) and Rockaway (N.Y.), and a second on the upper East River to provide a ring of protection to most of the bi-state region. Through extensive use of floodgates, both barriers would have largely open cross-sections during normal conditions to minimize environmental impacts on the estuary and port operations. [1]

Contents

Alternatively the southern barrier could be located between Coney Island and Staten Island. A storm surge barrier at this location would be half as long, but would require supplemental barriers across the entrances to Jamaica Bay and the Arthur Kill. [2]

To address the problem of sea level rise, smaller scale projects to increase seawall heights or otherwise raise vulnerable coastlines would be necessary. Thus a storm-surge barrier system combined with coastline adjustments would form a two-tiered strategy to protect the region. The barrier system could also be extended eastward, filling in the gaps between barrier islands, to protect the various communities lining the south shore of Long Island.

External videos
Nuvola apps kaboodle.svg Video animation of originally proposed Outer Harbor Barrier in operation (4:11).
Nuvola apps kaboodle.svg Video animation of Verrazano Barrier's more open design (0.30).

The proposal was developed in the wake of Hurricane Sandy by the Metropolitan NY-NJ-LI Storm Surge Working Group (SSWG), composed of prominent civic leaders, social scientists, oceanographers, engineers, and architects. The group is chaired by Malcolm Bowman, a professor of physical oceanography at the State University of New York at Stony Brook. [3] [4] Within the barrier system lies crucial infrastructure such as the seaports and maritime facilities; ground level and underground transportation terminals; three major international airports; subway and roadway tunnels; hospitals; communication centers; the industrial complex of northern New Jersey; as well as the millions of residents at risk in New York City and coastal New Jersey north of Sandy Hook. [5]

Need

The New York-New Jersey Harbor is vulnerable to storm surges that threaten to inundate the region, put in danger large numbers of the metropolitan area's residents, devastate much critical infrastructure and damage some of its most important economic assets. At particular risk are the most vulnerable, low-income communities located in many public housing projects located on low-lying land near to the coast. [6]

The source of energy for all hurricanes is the elevated temperatures of the tropical Atlantic Ocean and the associated warm surface temperatures of the Gulf Stream flowing northwards along the eastern seaboard. Accordingly, hurricanes are most dangerous when their track lies slightly offshore. [7]

Sandy 2012 track Sandy 2012 track.png
Sandy 2012 track

Hurricane Sandy's power came from unusually warm water lying off the mid-Atlantic Coast and the merging of two major storm systems. Technically, Sandy was downgraded from a category one hurricane to an extra-tropical storm just before it made landfall in New Jersey on October 29, 2012. Nevertheless, as the largest storm in extent ever recorded by the National Weather Service (at 1100 miles in diameter), Sandy's storm-surge impacts on New York and New Jersey were severe. [6]

Because of global warming, oceanographic and meteorological experts currently predict that increasingly warmer future ocean surface temperature is the "new normal", implying that extreme weather events like Hurricanes Sandy and Maria could become more intense and possibly more frequent during future hurricane seasons. As the world's oceans steadily become warmer; storms are becoming stronger and larger. These storms will cause more damage if they follow past storm tracks. [7] [8] For example, research suggests that hurricanes that have hit the New York City area since 1970 are more intense or have larger wind fields, producing higher storm surge and flood risk. When added to rising sea level, what was a 500-year flood event before the anthropogenic era (i.e. pre-1800) is now a 24-year flood event [9] and in 30 years will be a 5-year flood event. [10] [11]

The risks to the New York Metropolitan Region also include wind and flooding damage from winter nor’easter storms which can be as serious, or even more dangerous, than rarer hurricanes. While hurricanes are short and violent, nor’easters tend to persist longer for several days also producing large storm surges that ride atop successive high tides that occur twice daily. [6]

Adding to storm surge risks, sea levels are also rising. Over the last 160 years the National Oceanic and Atmospheric Administration's (NOAA's) Battery Park tide gauge has measured the rate of sea-level rise as one foot per century. [12] But sea level rise has begun to accelerate, potentially adding an additional 36 feet to current sea level by the end of this century, or possibly more if the melting of the Greenland ice sheet continues at ever increasing rates and huge chunks of ice around Antarctica continue to break off. [7] [10] [13] [14] [15] [16]

Precedents

Maeslant Barrier, the Netherlands Maeslantkering.jpg
Maeslant Barrier, the Netherlands

Similar, albeit more modestly-sized, but still highly effective storm-surge barriers have been in operation for nearly half a century in three New England communities — the Stamford Hurricane Protection Barrier in Stamford, Conn.; the Fox Point Hurricane Barrier in Providence, R.I.; and the New Bedford Harbor Hurricane Barrier [17] in New Bedford, Mass. Hours before Hurricane Sandy struck Stamford, the city's 17-foot-high movable barrier was closed to withstand an over-11-foot storm tide which struck western Long Island Sound (at some locations on the sound, the storm tide was even higher than the 11.5-foot storm tide measured at The Battery in New York City), devastating every waterfront community on the northwestern coast of the sound — except Stamford. [18] [19]

Larger barrier systems protect more than a dozen major cities, including the Delta Works protecting the south of the Netherlands and the MOSE Project protecting Venice. New storm-surge barriers on Lake Borgne and Lake Pontchartrain are part of the protection for New Orleans after Hurricane Katrina.

The famous Thames Barrier is typically deployed an average of about twice per year, protecting the heart of London from excessive tidal flooding. The Greater London Authority is currently studying proposals to strengthen its defenses.

Flooding in St. Petersburg, Russia during the 1824 flood 7 noiabria 1824 goda na ploshchadi u Bol'shogo teatra.jpg
Flooding in St. Petersburg, Russia during the 1824 flood

The new Saint Petersburg Dam was built to stop the frequent floods in the city, which had often devastated the city. It was first used on November 28, 2011, just months after it was completed, and limited storm water rise to below flood level. [20] It prevented the 309th flood in the history of the city. [21]

Background

During the same period when the New England storm surge barriers were built, the Army Corp of Engineers warned of possible catastrophic storm surge flooding in New York City and discussed a possible storm surge barrier system for New York Harbor. [22] However there was little local interest in such a project. [23]

With funding from the Rockefeller Foundation, Mayor Michael Bloomberg, convened the New York City Panel on Climate Change in August 2008 to investigate the city's vulnerability to a variety of climate-induced risks including the risk of a major storm-surge event. At about the same time, the American Society of Civil Engineers organized a three-day conference and subsequently published a report entitled "Storm-Surge Barriers to Protect New York City Against the Deluge." [24] [25] [26]

After Hurricane Sandy devastated the New York - New Jersey metropolitan area in 2012, governments struggled both to recover and to plan better protection for the future, including regional storm-surge barriers. In his January 2013, State of the State address, [27] New York Governor Andrew Cuomo proposed to "work with other government partners to timely complete a comprehensive engineering evaluation of these potential barrier systems."

The City of New York, under Mayor Michael Bloomberg, organized a "Special Initiative for Rebuilding and Resiliency" (SIRR), which developed a blueprint for reconstruction that was released in June 2013, only eight months after the storm. That over-400-page document describes the demographics and morphology of the region, the storm and its impacts; provides background on extreme weather events including non-storm events such as heat and intense rainfall; describes various resiliency measures and strategies; and describes specific initiatives, studies and projects to be undertaken. [6] Some of these projects are underway, using a combination of federal and local funds. [28] [29] [30] [31] [32]

City and regional response

Despite Governor Cuomo's announced interest in storm surge barriers, Mayor Bloomberg was reluctant to proceed. [33] [34] [35] But the City asked Dr. Jeroen Aerts, a professor of water and climate risk with the VU University of Amsterdam, the Netherlands, and an expert on water risk management, to compare the costs and benefits of a regional barrier system with those of smaller-scale changes like building levees around sewage treatment plants, raising subway stations entrances, constructing local storm-surge barriers, and flood-proofing or raising buildings according to the FEMA-run National Flood Insurance Program standards. [18] [36] [37] At the same time FEMA intends to redraw flood maps for New York City, placing a much larger area in the flood zone. [38]

Dr. Aerts' report indicated that, assuming a middle scenario for climate change, which includes the combined effect of sea-level rise and increased storm activity, the benefit/cost ratio of investment in a regional barrier would be similar to the ratio for investment in smaller-scale changes. [39] Despite that result, the city's SIRR report dismissed the regional barrier idea without any further study. The report listed seven reasons for doubt about the feasibility: [6]

  1. Such a system of barriers would be extraordinarily expensive — perhaps costing $20–25 billion to build.
  2. Harbor-wide barriers would require a design, approval and construction process that could take two to three decades to complete.
  3. The possible hydrodynamic and environmental impacts on fish migration, siltation, river flow, and water quality are likely to be substantial and are not yet known.
  4. To make the project work, massive levees along adjacent coastal areas, including on the Rockaway Peninsula and possibly Coney Island and Staten Island would have dramatic impacts on the character of the beaches and adjacent neighborhoods that may prove to be highly disruptive.
  5. Any barriers would create an “insiders/outsiders” dynamic, with only those behind the barriers receiving maximum protection, leaving densely developed communities along the South and North Shores of Long Island and the Jersey Shore outside the protected zone.
  6. A harborwide barrier project may also cause additional flooding in areas outside the barriers, making those communities more vulnerable than they would be without such barriers.
  7. Finally, since the barriers would be open most of the time (to allow navigation), it would represent a major public investment that would end up doing nothing to address the growing problem of rising sea level.
External media
Images
Searchtool.svg Map showing SIRR Phase 1 coastal protection plan.
Searchtool.svg Map showing SIRR full coastal protection plan.
Searchtool.svg Map showing areas vulnerable to sea-level rise
Searchtool.svg Map showing housing units vulnerable to sea-level rise.
Video
Nuvola apps kaboodle.svg PBS News Hour segment on how New York City is preparing for future hurricanes, October 28, 2013 (8:16).
Nuvola apps kaboodle.svg PBS News Hour segment on Dutch lessons for protecting New York Harbor, Oct 29, 2013 (8:39).

Instead of a barrier system, the SIRR report identified a plethora of local measures that could be taken by the city. The goal of these measures is to protect vulnerable areas of the city with projects that would be relatively inexpensive, effective and quickly designed and constructed. They include local walls or barriers against storm surge on some sections of the coast. [6] [40] For example, a barrier has been funded as part of an inner defensive ring for Lower Manhattan, [41] to be integrated into the Manhattan Waterfront Greenway.

At the same time that the city was implementing its own local flood mitigation strategy, the MTA, Port Authority of New York and New Jersey and many major institutions and private companies adopted their own localized plans for their facilities. Hoboken and other cities in the region have initiated their own local measures, [42] [43] with support from the U.S. Department of Housing and Urban Development's Rebuild by Design competition. [44] The U.S. Army Corps of Engineers has conducted coastal storm risk reduction studies and beach restoration and resiliency projects. [45] [46]

Because of the variety of governmental entities involved, as well as differing community reaction, there is a lack of coordination on goals and standards of storm protection among the various projects. As a result, these scattered efforts have proved to be more difficult to execute, as well as more expensive than expected, and raise doubt about how much of the shoreline will be protected in the end. [47] [48] [49]

Counterarguments

Lost in all this activity is the conclusion of Dr. Aerts' study — that because of the expectation of rising sea level and increased global warming, by 2040 the benefit/cost ratio of a regional barrier system will far exceed the ratio for the measures the city is now taking, that a regional barrier may be needed soon, and that planning for it should begin now. [39] "As a Dutchman," Dr. Aerts said, "you are quite surprised íto see a large city like New York so many people exposed and no levees, no protection at all. [That] was astonishing to me. . . . Don't rule out yet the barriers because the sea level is going to rise very quickly, and then you need a barrier." [50] [51]

The Storm Surge Working Group has provided answers to all the objections raised by the city. [52]

  1. A barrier system would be expensive, but the city's plan, covering many miles of vulnerable coastline, would be even more expensive. And some of the cost to shore up areas on the sides of the barriers are scheduled to be spent anyway, for example in dune-building projects on the Rockaway peninsula and on Staten Island. [39] [45]
  2. If a barrier takes a long time to implement, so do local projects. More than ten years since Sandy struck, local projects have yet to be completed and have experienced the same problems (costs, public resistance, etc.) that were attributed to the regional storm surge barrier approach. [52]
  3. With regard to environmental impacts, the barriers' floodgates would be closed only for a few hours before, during and immediately after a major storm surge. Over 99% of the time, floodgates would remain open so as to minimally hinder tides, harbor flushing, river discharge, fish migration and healthy marine ecosystem functioning. An environmental impact study would evaluate whether any hindrance posed by the structure is outweighed by its benefit. Preliminary studies sponsored by the Hudson River Foundation indicate that an outer harbor barrier would minimally decrease tidal flow as long as floodgates allow at least 60% of the barrier cross section to be normally-open. [53] Even that small decrease merely offsets the equally small increase in tidal flow that resulted from digging shipping channels into the harbor over the past 150 years. [54]
  4. Reinforced dunes (not levees) will indeed have to be built in the Rockaways and Sandy Hook, and along Coney Island and Staten Island if the alternative barrier location is chosen. In fact in the wake of Hurricane Sandy reinforced dunes are already under construction on the Rockaway Peninsula and Staten Island. [55]
  5. Because of the immense lengths of the New York Bight and Atlantic shorelines (Montauk Point, N.Y. to Cape May, N.J.), research has shown that ocean water displaced by the barrier system would only increase coastal surges adjacent to the barrier by a few inches on the ocean and western Long Island Sound sides. [52]
  6. While ocean shore communities outside the region would not be protected by two or three barriers around New York Harbor, it may be possible to extend the area to be protected by constructing barriers in gaps between barrier islands along the south shore of Long Island, and south along the Jersey shore, or with barriers oriented perpendicular to the barrier islands, depending on the dominant direction of hurricane winds. [52] [56] [57]
  7. With normally-open storm-surge gates, barriers alone will not address sea level rise, but neither will local shoreline storm-surge projects planned by New York City, which will also have gates. The SIRR report, itself, found that by the 2050s 43 miles, or about 8%, of the city's coastline could be at risk of flooding during non-storm conditions. These coastal areas will need to be raised or otherwise protected regardless of additional protections against storm surge. [6]

The two-tiered approach of protecting local coastal areas against slowly changing sea level rise, together with 25-foot offshore barriers to hold back surges of future storms, will give future civic leaders 100 to 150 years to protect, and if necessary migrate, our urban metropolitan civilization to higher ground, and to adopt even more sweeping measures to protect the region from both sea level rise and storm surges. [52]

Another objection to barriers is that restored natural systems, such as created wetlands and oyster beds could provide the same protection. While these proposed solutions should be included in local responses because they can reduce wave action slightly, reinforce presently fragile wetlands and in some cases improve water quality, the reality is that they would be simply overwhelmed by storm surges of the magnitude experienced during Sandy. One naturalistic feature can resist storm-surge—levees or dunes. In fact most of the coastline of the Netherlands is protected in this way. [52] A regional storm surge barrier would depend on dunes along the coast of the Rockaway Peninsula and Sandy Hook, or, for the alternative location, along the coast of Staten Island.

Army Corps of Engineers study

External images
Searchtool.svg Map showing USACE Alt. 2 barriers and areas protected.
Searchtool.svg Map showing USACE Alt. 3A barriers and areas protected.
Searchtool.svg Map showing USACE Alt. 3B barriers and areas protected.
Searchtool.svg Map showing USACE Alt. 4 barriers and areas protected.
Searchtool.svg Map showing USACE Alt. 5 barriers and areas protected.

In the Fall of 2017, the U.S. Army Corps of Engineers (USACE) initiated a Coastal Storm Risk Management Feasibility Study [58] to evaluate various proposals to address storm surge in the New York and New Jersey harbor area. The New York Harbor Storm-Surge Barrier, modified to increase permeability, is represented by two of five alternatives being considered.

In December, 2020, Congress instructed the USACE to expedite the study, [59] after the Corps had "indefinitely postponed" the project the previous February. [60] The Biden Administration subsequently restarted by the study. A draft Feasibility Report and tier 1 environmental impact study is posted on the USACE website, [58] along with appendices.

To solicit comments on the choice of Alternative 3B as the Tentatively Selected Plan (TSP), the Corps has released a GIS-based summary, [61] a slide presentation, [62] and meeting posters. [58] In response, the Storm Surge Working has published a comprehensive layered flood defense strategy, [63] including a critique of the Corps' TSP.

The TSP is essentially a subset of the SIRR's shoreline barrier proposals for New York City with the addition of a floodwall around the Jersey City waterfront district and storm surge barriers at the entrances to Arthur Kill and Kill Van Kill to protect much of northern New Jersey. [2]

The schedule for the study is as follows:

Study InitiationLate 2016
NEPA Scoping PeriodFeb. 2018 - Nov. 2018
Release of the Interim ReportFeb. 2019
Delay due to funding suspensionFeb., 2020 – Sept., 2021
Tentatively Selected Plan (TSP)May, 2022
Draft Feasibility Report and Tier 1 EISSept. - Oct., 2022
Agency Reviews and Public MeetingsNov., 2022 – Mar., 2023
Agency Consultations and Confirmation of the TSPOct. 2023, Postponed
Final Feasibility Report and NEPA DocumentationTo be determined
Chief's ReportTo be determined
Pre-Construction Engineering and Design Phase & Tier 2 EIS

See also

Related Research Articles

The Delta Works is a series of construction projects in the southwest of the Netherlands to protect a large area of land around the Rhine–Meuse–Scheldt delta from the sea. Constructed between 1954 and 1997, the works consist of dams, sluices, locks, dykes, levees, and storm surge barriers located in the provinces of South Holland and Zeeland.

<span class="mw-page-title-main">Jamaica Bay</span> Bay on the southern side of Long Island, New York

Jamaica Bay is an estuary on the southern portion of the western tip of Long Island, in the U.S. state of New York. The estuary is partially man-made, and partially natural. The bay connects with Lower New York Bay to the west, through Rockaway Inlet, and is the westernmost of the coastal lagoons on the south shore of Long Island. Politically, it is primarily divided between the boroughs of Brooklyn and Queens in New York City, with a small part touching Nassau County.

<span class="mw-page-title-main">Storm surge</span> Rise of water associated with a low-pressure weather system

A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the normal tidal level, and does not include waves.

<span class="mw-page-title-main">New York–New Jersey Harbor Estuary</span> One of the most intricate natural harbors in the world

The New York–New Jersey Harbor Estuary, also known as the Hudson-Raritan Estuary, is in the northeastern states of New Jersey and New York on the East Coast of the United States. The system of waterways of the Port of New York and New Jersey forms one of the most intricate natural harbors in the world and one of the busiest ports of the United States. The harbor opens onto the New York Bight in the Atlantic Ocean to the southeast and Long Island Sound to the northeast.

<span class="mw-page-title-main">Seawall</span> Form of coastal defence

A seawall is a form of coastal defense constructed where the sea, and associated coastal processes, impact directly upon the landforms of the coast. The purpose of a seawall is to protect areas of human habitation, conservation, and leisure activities from the action of tides, waves, or tsunamis. As a seawall is a static feature, it will conflict with the dynamic nature of the coast and impede the exchange of sediment between land and sea.

<span class="mw-page-title-main">New York Bight</span> Coastal embayment south of Long Island and east of New Jersey

The New York/New Jersey Bight is the geological identification applied to a roughly triangular indentation, regarded as a bight, along the Atlantic coast of the United States that extends northeasterly from Cape May Inlet in New Jersey to Montauk Point on the eastern tip of Long Island. As the result of direct contact with the Gulf Stream along the coast of North America, the coastal climate of the bight area is temperate.

<span class="mw-page-title-main">Hurricane preparedness in New Orleans</span>

Hurricane preparedness in New Orleans has been an issue since the city's early settlement because of its location.

<span class="mw-page-title-main">Flood barrier</span> Floodgate designed to prevent a storm surge

A flood barrier, surge barrier or storm surge barrier is a specific type of floodgate, designed to prevent a storm surge or spring tide from flooding the protected area behind the barrier. A surge barrier is almost always part of a larger flood protection system consisting of floodwalls, levees, and other constructions and natural geographical features. Flood barrier may also refer to barriers placed around or at individual buildings to keep floodwaters from entering the buildings.

<span class="mw-page-title-main">Flood management</span> Methods for reducing detrimental effects of flood waters

Flood management describes methods used to reduce or prevent the detrimental effects of flood waters. Flooding can be caused by a mix of both natural processes, such as extreme weather upstream, and human changes to waterbodies and runoff. Flood management methods can be either of the structural type and of the non-structural type. Structural methods hold back floodwaters physically, while non-structural methods do not. Building hard infrastructure to prevent flooding, such as flood walls, is effective at managing flooding. However, it is best practice within landscape engineering to rely more on soft infrastructure and natural systems, such as marshes and flood plains, for handling the increase in water.

<span class="mw-page-title-main">IHNC Lake Borgne Surge Barrier</span> Bridge in New Orleans, Louisiana

The Inner Harbor Navigation Canal Lake Borgne Surge Barrier is a storm surge barrier constructed near the confluence of and across the Gulf Intracoastal Waterway (GIWW) and the Mississippi River Gulf Outlet (MRGO) near New Orleans. The barrier runs generally north-south from a point just east of Michoud Canal on the north bank of the GIWW and just south of the existing Bayou Bienvenue flood control structure.

<span class="mw-page-title-main">Seabrook Floodgate</span> Bridge in New Orleans, Louisiana

The Inner Harbor Navigation Canal (IHNC) Seabrook Floodgate Structure is a flood barrier in the Industrial Canal in New Orleans, Louisiana. The floodgate is designed to protect the Industrial Canal and the surrounding areas from a storm surge from Lake Pontchartrain. It consists of two 50-foot (15 m) wide vertical lift gates and a 95-foot (29 m) wide sector gate.

<span class="mw-page-title-main">Coastal flooding</span> Type of flooding

Coastal flooding occurs when dry and low-lying land is submerged (flooded) by seawater. The range of a coastal flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding. The seawater can flood the land via several different paths: direct flooding, overtopping or breaching of a barrier. Coastal flooding is largely a natural event. Due to the effects of climate change and an increase in the population living in coastal areas, the damage caused by coastal flood events has intensified and more people are being affected.

<span class="mw-page-title-main">Effects of Hurricane Sandy in New York</span>

New York was severely affected by Hurricane Sandy on October 29–30, 2012, particularly New York City, its suburbs, and Long Island. Sandy's impacts included the flooding of the New York City Subway system, of many suburban communities, and of all road tunnels entering Manhattan except the Lincoln Tunnel. The New York Stock Exchange closed for two consecutive days. Numerous homes and businesses were destroyed by fire, including over 100 homes in Breezy Point, Queens. Large parts of the city and surrounding areas lost electricity for several days. Several thousand people in midtown Manhattan were evacuated for six days due to a crane collapse at Extell's One57. Bellevue Hospital Center and a few other large hospitals were closed and evacuated. Flooding at 140 West Street and another exchange disrupted voice and data communication in lower Manhattan.

<span class="mw-page-title-main">Hurricane & Storm Damage Risk Reduction System</span>

The greater New Orleans Hurricane & Storm Damage Risk Reduction System (HSDRRS) is an infrastructure system in southern Louisiana which seeks to provide the greater New Orleans area a 100-year level of risk reduction, meaning reduced risk from a storm surge that has a 1% chance of occurring or being exceeded in any given year. In 2019, the Army Corps of Engineers announced that due to an increased rate of sea level rise and continued sinking of soil the levee system would no longer offer original planned levels of protection as early as the year 2023.

<span class="mw-page-title-main">Sea Bright–Monmouth Beach Seawall</span> Seawall in New Jersey

The Sea Bright–Monmouth Beach Seawall is a seawall located along the Jersey Shore in the Monmouth County, New Jersey towns of Sea Bright and Monmouth Beach. It roughly runs north-south direction along 4.7 miles (7.6 km) of the barrier spit of land along the lower Sandy Hook peninsula between the Atlantic Ocean and the Shrewsbury River estuary. The use of seawalls, groins, jetties, bulkheads, revetment, and beach nourishment since the late 1800s has made the stretch of coast one of the most heavily engineered sections of ocean shorefront in the world.

<span class="mw-page-title-main">Climate change in Virginia</span> Climate change in the US state of Virginia

Climate change in Virginia encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Virginia.

<span class="mw-page-title-main">Climate change in New Jersey</span> Climate change in the US state of New Jersey

Climate change in New Jersey is of concern due to its effects on the ecosystem, economy, infrastructure, and people of the U.S. state of New Jersey. According to climatology research by the U.S. National Oceanic and Atmospheric Administration, New Jersey has been the fastest-warming state by average air temperature over a 100-year period beginning in the early 20th century, related to global warming.

<span class="mw-page-title-main">Sinking cities</span> Cities endangered by environmental change

Sinking cities are urban environments that are in danger of disappearing due to their rapidly changing landscapes. The largest contributors to these cities becoming unlivable are the combined effects of climate change, land subsidence, and accelerated urbanization. Many of the world's largest and most rapidly growing cities are located along rivers and coasts, exposing them to natural disasters. As countries continue to invest people, assets, and infrastructure into these cities, the loss potential in these areas also increases. Sinking cities must overcome substantial barriers to properly prepare for today's dynamic environmental climate.

<span class="mw-page-title-main">Land reclamation in Lower Manhattan</span> Landfilling of Lower Manhattan, NYC

The expansion of the land area of Lower Manhattan in New York City by land reclamation has, over time, greatly altered Manhattan Island's shorelines on the Hudson and East rivers as well as those of the Upper New York Bay. The extension of the island began with European colonialization and continued in the 20th century. Incremental encroachment, landfill, as well as major infrastructure have added acreage to the island. Since the passage of the Rivers and Harbors Act of 1899 all projects which extend into navigable waterways follow federal regulation and are overseen by the United States Army Corps of Engineers.

<span class="mw-page-title-main">East Shore Seawall</span>

The East Shore Seawall, also known as Staten Island Multi-Use Elevated Promenade, is a 5.2-mile (8.4 km) long combined seawall and esplanade proposed for the eastern shoreline of Staten Island, New York. It would run along the Lower New York Bay linking sections of the Gateway National Recreation Area: Fort Wadsworth at the north, Miller Field, and Great Kills Park to the south. It will roughly parallel Father Capodanno Boulevard and the South Beach–Franklin Delano Roosevelt Boardwalk.

References

  1. Barnard, Anne (January 17, 2020). "The $119 Billion Sea Wall That Could Defend New York … or Not". The New York Times.
  2. 1 2 Robert Yaro and Daniel Gutman, "The Plan to Save New York From the Next Sandy Will Ruin the Waterfront. It Doesn’t Have To.," New York Times, June 15, 2023
  3. Malcolm Bowman's biography.
  4. Patrick McGeehan, Making a Pitch, Again, for Barriers to Block Storm Surges," New York Times, October 11, 2017.
  5. Henry Goldman, "New York City Planners With Sandy Nightmares Say Barrier May Come Too Late," Bloomberg News, June 20, 2017.
  6. 1 2 3 4 5 6 7 City of New York, "PlaNYC, A Stronger, More Resilient New York", June 11, 2013.
  7. 1 2 3 New York Academy of Sciences, "New York City Panel on Climate Change 2015 Report", Ann. N.Y. Acad. Sci. ISSN 0077-8923, January 2015.
  8. Lin, et al., "Hurricane Sandy's flood frequency increasing from year 1800 to 2100,", PNAS 113 (43) 12071.
  9. Andra J. Reed, et al., "Increased threat of tropical cyclones and coastal flooding to New York City during the anthropogenic era,", PNAS 112 (41) 12610-12615, October 28, 2015.
  10. 1 2 Andra J. Garner, et al., "Impact of climate change on New York City's coastal flood hazard: Increasing flood heights from the preindustrial to 2300 CE,", PNAS 114 (45) 11861, November 7, 2017.
  11. Stefan Rahmstorf, "Rising hazard of storm-surge flooding," PNAS, 114 (45) 11806-11808, November 7, 2017.
  12. NOAA, Battery Park Mean Sea Level Trend.
  13. James Hanson, "Why I Must Speak Out about Climate Change," TED Talk, 2012.
  14. Damian Carrington, "Sea levels set to 'rise far more rapidly than expected.'" The Guardian, March 30, 2016.
  15. Don Jergler, "RIMS 2016: Sea Level Rise Will Be Worse and Come Sooner," Insurance Journal, April 12, 2017.
  16. David Wallace-Wells, "The Uninhabitable Earth: Famine, economic collapse, a sun that cooks us: What climate change could wreak — sooner than you think," New York Magazine, July 9, 2017.
  17. U.S. Army Corps of Engineers, "New Bedford Hurricane Protection Barrier".
  18. 1 2 Mireya Navarro, New York Times, "Weighing Sea Barriers as Protection for New York", November 7, 2012.
  19. Andrew Morang, "Hurricane Barriers in New England and New Jersey: History and Status after Five Decades," Journal of Coastal Research, 32 181–205 (2016).
  20. (in Russian) Мощнейший ураган и наводнение накрыли Петербург: вода угрожает городу (ВИДЕО), Главред, November 28, 2011
  21. "Дирекция КЗС: Дамба предотвратила ущерб в 1,3 млрд рублей". fontanka.ru - новости Санкт-Петербурга. November 29, 2011.
  22. Samuel Gofseyeff and Frank L. Panuzio, "Hurricane Studies of New York Harbor," Transactions of the American Society of Civil Engineers, 128 (1963).
  23. John C. Devlin, "U.S. Survey Sees City Flood Peril," New York Times, October 18, 1961.
  24. Malcolm J. Bowman, "A City at Sea," New York Times, September 25, 2005.
  25. D. Hill. M.J. Bowman, J.S. Khinda, "Storm Surge Barriers to Protect New York City: Against the Deluge,” 2012.
  26. James Glanz and Mireya Navarro, "Engineers’ Warnings in 2009 Detailed Storm Surge Threat to the Region," New York Times, November 4, 2012.
  27. Governor Andrew Cuomo, "NY RISING: 2013 State of the State", October 29, 2012.
  28. Lisa W. Foderaro, "In Rockaways Infusion of Sand Will Soon Raise Beaches Hit by Hurricane Sandy," New York Times, February 28, 2014.
  29. Nathan Kensinger, "Four years after Sandy, Staten Island's shoreline is transformed," Curbed, October 27, 2016.
  30. Nathan Kensinger, "Climate change in Trump's NYC: How at-risk neighborhoods are combating rising sea levels," Curbed, January 26, 2017.
  31. Nathan Kensinger, "A long-neglected Queens neighborhood grapples with the effects of climate change in NYC," Curbed, April 13, 2017.
  32. Luis FERRÉ-SADURNÍ, "Could the Rockaways Survive Another Sandy?" New York Times, July 13, 2007.
  33. Joe Nocera, "Mayor Bloomberg's Barrier," New York Times, November 3, 2012.
  34. ABC News, "Sandy Spurs Talk of Sea Barrier for New York," November 2, 2012
  35. WCBS, Bloomberg on Storm Barrier Idea: Not in Your Lifetime." March 5, 2013.
  36. David W. Dunlap, "A Guide to Flood-Resistant Building," New York Times, January 25, 2017.
  37. Brooke Jarvis, "When Rising Seas Transform Risk Into Certainty," New York Times, April 18, 2017.
  38. David W. Chen, "In New York, Drawing Flood Maps Is a 'Game of Inches'," New York Times,January 7, 2018.
  39. 1 2 3 Jeroen Aerts, et al., "Evaluating Flood Resilience Strategies for Coastal Megacities", Science, 344:473, May 2, 2014.
  40. David W. Dunlap, "Building to the Sky, With a Plan for Rising Waters," New York Times, January 26, 2017.
  41. "Lower Manhattan flood barrier gets $176M in fed funds". NY Daily News. Retrieved August 14, 2017.
  42. Patrick McGeehan, "Plan to Flood-Proof Hoboken Runs into a Wall," New York Times, February 7, 2016.
  43. Ford Fessenden and Jeremy White, "Hoboken Flood Wall Maps," New York Times, February 7, 2016.
  44. Kia Gregory, "HUD Storm Protection Competition Will Narrow Ideas Big and Small," New York Times, November 14, 2013.
  45. 1 2 U.S. Army Corps of Engineers. "NY District Coastal Storm Risk Reduction Projects and Studies Map" . Retrieved April 19, 2017.
  46. Mireya Navarro and Rachel Nuwer, "Resisted for Blocking the View, Dunes Prove They Blunt Storms," New York Times, December 12, 2012
  47. Marc Santora, "Scientists Glimpse New York's Perilous Path in an Ancient Patch of Marsh," New York Times, January 19, 2017.
  48. Justin Davidson, "Sea Levels Might Be Rising Much Faster Than Expected. What Should New York Do to Avoid Being Swamped?," New York Magazine, July 23, 2015.
  49. Josh Robbin, "Five Years After Sandy: Blown Deadlines," NY1, October 25, 2017.
  50. PBS News Hour segment on Dutch lessons for protecting New York Harbor, Oct 29, 2013 (8:39).
  51. Michael Kimmelman, The Dutch Have Solutions to Rising Seas. The World Is Watching." New York Times, June 15, 2017.
  52. 1 2 3 4 5 6 Storm Surge Working Group, "Protecting the NY-NJ Metropolitan Region from The Next Disastrous Storm Surge: Summary Report," December 29, 2016.
  53. David K. Ralston, "Impacts of storm surge barriers on drag, mixing, and exchange flow in a partially mixed estuary," J. Geophys. Res., 127 April, 2022.
  54. David Ralston, et al., "Bigger tides, less flooding: Effects of dredging on barotropic dynamics in a highly modified estuary," J. Geophys. Res., 124, 196-211 (2019).
  55. USACE New York projects
  56. "USACE New Jersey Back Bays Study, 2021". www.nap.usace.army.mil.
  57. USACE, Nassau County Back Bays Study, 2021.
  58. 1 2 3 NY & NJ Harbor & Tributaries Focus Area Feasibility Study (HATS)
  59. "Waterfront Alliance Press Release" (PDF).
  60. Barnard, Anne (February 25, 2020). "After Trump Mocks a Sea Wall in New York, Plan Is Abruptly Shelved". The New York Times. ISSN   0362-4331 . Retrieved February 27, 2020.
  61. "NYNJHAT Study StoryMap". hats-cenan.hub.arcgis.com.
  62. January 2023 HATS Presentation
  63. Storm Surge Working Group, Regional Layered Flood Defense Strategy, August 2024.