storm surges – Techso Mogro https://techsomogro.com/ Science, Technology and the Future Tue, 23 Dec 2014 20:17:51 +0000 en-US hourly 1 https://wordpress.org/?v=6.8.1 Miami Beach’s Answer to Rising Sea Levels – More Waterfront Condos https://techsomogro.com/miami-beachs-answer-rising-sea-levels-waterfront-condos/?utm_source=rss&utm_medium=rss&utm_campaign=miami-beachs-answer-rising-sea-levels-waterfront-condos https://techsomogro.com/miami-beachs-answer-rising-sea-levels-waterfront-condos/#respond Tue, 23 Dec 2014 20:17:51 +0000 http://www.21stcentech.com/?p=16013 December 23, 2014 – Southern Florida is the most vulnerable floodplain in the United States. The City of Miami Beach to protect itself from storm surges is attempting to implement a $300 million deflection project. But to get the money it needs to collect more taxes. And where is it getting these taxes from? Development fees and taxes from builders.

Florida collects no state income tax. Property taxes, therefore, are the only means to fund infrastructure development. So to get property tax revenues up the city is permitting shoreline property developers to build 47 new condominiums in Miami Beach. And people are buying.

 

Miami Beach development

 

Consider what climate scientists are predicting for South Florida as sea levels continue to rise from a warming ocean and melting polar glaciers and sea ice. One climatologist, David Zierden, at Florida State University, recently stated “When you consider current hurricane threats, and the sea level rise that could erode these properties….Common sense says no, you shouldn’t do it.”

The project Miami Beach has undertaken includes 80 storm pumps that can pump sea water back into Biscayne Bay at a rate of  53,000 liters (14,000 gallons) per minute. This may help to mitigate the current state of frequent flooding that occurs at high tide but will it withstand sea levels that rise by a mean average of 0.4 meters (1.3 feet) in the next 85 years? And that 0.4 meters rise is a low-end estimate representing a global mean. Recent research done at Florida State University suggests a much more dire predicament, a local sea level rise of 81 centimeters (32 inches).

Of course the numbers above only cover a calm sea. Storm surges both in winter and during hurricane season will actively erode the Miami Beach area far beyond the impacts of rising sea levels. A single storm surge of 50 centimeters (19 inches) today is close to half the average elevation of the City which stands at 1.2 meters (4 feet). Now imagine a higher sea level combined with a storm surge and the entire City could be inundated.

Today Miami Beach loses its beaches with great regularity after Atlantic Ocean storms. Sand is imported to keep up the appearance of continuity. But that is far from the case.

With the City celebrating its 100th birthday the question is, will it be around for the next one hundred?

 

Miami Beach storm surge

 

 

 

 

 

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Climate Change Update: Rebuilding Staten Island, the Jersey Shore, Long Island and Lower Manhattan https://techsomogro.com/climate-change-update-rebuilding-staten-island-jersey-shore-long-island-manhattan/?utm_source=rss&utm_medium=rss&utm_campaign=climate-change-update-rebuilding-staten-island-jersey-shore-long-island-manhattan https://techsomogro.com/climate-change-update-rebuilding-staten-island-jersey-shore-long-island-manhattan/#comments Thu, 08 Nov 2012 00:55:08 +0000 http://www.21stcentech.com/?p=7047 In 2007 New York City released a plan entitled PlaNYC. It focused on the future sustainability of the city and included a section dealing with climate change.  The key points focused on increasing the resilience of the city’s built and natural environments by:

  1. Developing strategies to encourage the use of flood protection in buildings.
  2. Protecting New York City’s critical infrastructure.
  3. Identifying and evaluating city-wide coast protective measures.
  4. Recognizing the potential destructiveness of coastal storms combined with the rise in sea level.

New York recognized not just waterfront property would be impacted by climate change and weather events. Flooding could immobilize 700 miles of subway, impact the 90,000 miles of underground power cables, compromise 14 wastewater treatment plants, and potentially cause a transportation nightmare if any of the 2,000 bridges and tunnels were damaged. All this infrastructure was immovable and a storm could make it vulnerable to massive disruption.

Enter Hurricane Sandy, a Category 1 storm that tested the city and its neighbouring shorelines like no other before it. Today in the aftermath of Sandy, the Atlantic coastline that includes New Jersey, Long Island and New York City is faced with a herculean task.

This map was created in 2011 to show what areas of Long Island and New York City were most vulnerable to storm surges. It is these areas in red, orange, yellow and green that Sandy inundated.

How do you prevent another storm from wreaking damage ($50 billion estimated so far) equal to or even greater than Sandy? If Sandy, a Category 1 hurricane could do this imagine what a Category 2 or 3 could co and then consider what kind of infrastructure would be needed to deal with such destructive storms.

What are the forces of nature we have to fight to keep the Atlantic Ocean at bay?

  1. Rising sea levels – In 2007 the IPCC projected global sea level rises of between 0.2 and 0.5 meters (approximately 8 to 20 inches)  by the year 2100.  But recent evidence according to the Geological Society of America is suggesting the projections are too low. Revisions suggest a high end of close to 1 meter (39 inches). So whether we take the low ball number or the revised number we are looking at higher water. See the graph below showing New York City harbour data on rising sea levels. It’s an eye opener.
  2. Storm surges and Local Geography – New York City sits at the apex of a funnel. A storm coming from the southeast will push Atlantic Ocean water into this narrowing space aided by a shallow and wide continental shelf. In addition, much of the shoreline is primarily composed of loose materials including sand, gravel and clay, all easily reworked by wind and water. Factor in all these characteristics and you have a recipe for a Sandy to do its worst.
  3. Storm Frequency Changes – In the last century the frequency of Atlantic hurricanes has doubled. Climatologists conclude that warmer ocean surface temperatures and altered wind patterns are the cause. Between 1900 and 1930, we averaged 6 tropical cyclones (not all at hurricane strength) per year. The frequency between 1995 and 2005 has reached an annual average of 15. Between 1900 and 2005 tropical ocean surface temperatures in the Atlantic have risen by 0.7 degrees Celsius (1.3 Fahrenheit).
  4. Storm Intensity Changes – Hurricane Sandy was a Category 1 when it struck the Jersey Shore. Hurricane Hazel which tracked over a similar path in 1954 was a Category 3. Hurricane Donna in 1960 was a Category 1 by the time it reached Long Island. So intensity seems to be highly variable with no correlation to rising ocean surface temperatures.
rising sea levels New York City
The plot seen above is a record of changing sea levels in the tidal estuary and harbour of New York City. Note the steady rise through the last century.
New York City is at the apex of a gradually inclined continental shelf that increases the height of storm surges. Staten Island, seen here in red on the left is most vulnerable to high water.

With Sandy it was much more than intensity, it was the immensity. And now this area has to rebuild. What should be done? Here are a number of initiatives that can harden the area to future storms and storm surges.

  1. Long Island and New Jersey need to re-engineer their shorelines to build them up to withstand Atlantic storms and rising sea levels.
  2. Flood gates need to be built on the approaches to New York City to counter storm surges
  3. New York City needs to develop flood defenses to ensure its infrastructure is not compromised.
  4. Buildings in coastal cities in New York and New Jersey need to develop self-sustaining capability to withstand a blackout from the grid going down.

Re-Engineering the Shoreline

Because of the nature of the material content of the New Jersey, Staten Island and Long Island shorelines beach replenishment is a non-starter. Just piling sand on top of the areas eroded by storm surge will do little to ensure the durability and duration of any repair. Not only that, the cost of pumping sand up from offshore where the hurricane dumped it can be quite prohibitive. Once you start down this path it becomes an ongoing exercise.

Another traditional coastline rehabilitation technology is the building of groins (seen below) and jetties. Although successful as sand traps they prove to be ineffective against storm surges turning shorelines into obstacle courses.

The most commonly used defense for storm surges includes the building of seawalls and levees. It was poorly maintained levees that allowed Katrina’s storm surge to flood New Orleans. Properly built and maintained they would have prevented that Category 3 hurricane from inundating much of the city. A series of seawalls on Long Island, Manhattan, Staten Island and the Jersey Shore all failed during Sandy. They were not built high enough or strong enough to withstand the storm surge. If rebuilding of the walls is to be done, engineers may want to consider defense in depth with a combination of berms or levees and well anchored taller walls.

The existing seawall infrastructure, Cape May, New Jersey on the left and Battery Park in Lower Manhattan, on the right, proved ineffective in combating Hurricane Sandy.

At best any beach shoreline re-engineering will prove a temporary fix as a line of defense against storm surges. It is the price of building on shifting sand.

Flood Gates

With 75% of the world’s population expected to be living in coastal communities by 2025 a more effective technology solution, than those described above, for combating rising ocean levels and storm surges is very much needed. And yet there are plenty of good examples of a technology that works already in place – flood gates. The Dutch have been building them for years allowing them to reclaim hundreds of square kilometers of land from the North Sea. The Thames River gates stave off potential flooding of London. Venice has been building new flood barriers to stop the Adriatic Sea from further damaging the city. Flood gates control the flow of the Mississippi River. And even New Orleans has them now to protect it from storm surges. So why not New York?

Storm surge flood gates strategically located at Arthur Kill, Verrazano Narrows and Throgs Neck would not protect the Jersey Shore or the south beaches of Long Island, but would control flooding in Manhattan, Brooklyn and the leeward side of Staten Island. The inset picture at the bottom shows the location of the gates in relation to the Verrazano Narrows Bridge.

The cost of such a project is estimated at $15 billion, less than one-third of the estimated cost for cleaning up the damage caused by Hurricane Sandy.

City Internal Defenses

One proposal that has come out of Hurricane Sandy includes the development of a giant inflatable plug that looks like something out of a Woody Allen comedy. You can see it in the picture below.

The plug is just under 10 meters in length (32 feet) and 5 meters wide (16 feet). It can be inserted deflated into a tunnel opening and then quickly filled with water to effectively seal it off. Made from Vectran, a liquid-crystal polymer fiber, several could be placed in strategic locations to protect subways, roadway tunnels and other vulnerable sub-structure. Each costs $400,000.

To protect smaller underground accesses such as ventilation shafts technology can be designed to automatically seal entrances in the advent of a storm surge, further protecting New York’s infrastructure from flooding.

Building for Off the Grid

Urban living is heavily reliant on the energy grid. When it goes down it’s more than lights out. Elevators are inoperable. Appliances no longer work. Water pressure falls and without supplementary pumps is no longer available to apartment dwellers. Add to this the loss of transit like subways which rely on electricity and you have a pretty dysfunctional urban setting. That’s why cities like New York need to develop sustainable energy technology for high rise buildings in the event of a prolonged loss of power from the energy grid.

This can be accomplished using renewable energy sources like solar and wind. Apartment waste can be converted to energy using small cookers to heat water to drive turbines. Apartments could be outfitted with supplementary battery storage to cover the gaps when the sun is not shining or the wind not blowing. This would ensure continuous power for operating essential services such as elevators, air conditioning, common area lighting and water pumps.

Some buildings today in New York City are installing Otis “Gen2” elevators that use 75% less energy by feeding energy recovered from braking during descent and feeding it into the building’s internal electrical grid. Other innovations include blue roofs designed to capture rainwater for use in sanitation. A typical New York building outfitted this way could capture thousands of cubic meters of water for lots of low-flow toilet flushes.

 

 

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