Until a few years ago, Hunter’s Point South Waterfront Park in Long Island City, Queens, was an industrial landfill. Now it’s a modern-day version of the marshes that once flanked the East River, with a running path that zigzags along the water’s edge atop a grassy berm, and an inlet filled with marsh grasses to let water flow in and out with the tides.
The park, completed in 2017, is also a fortification. The marshland is designed to absorb flooding from storms and sea-level rise, while hills, berms, and concrete walls block or redirect floodwaters to protect the neighborhood.
Nearly seven years ago, the swollen river flooded Long Island City during Superstorm Sandy, pouring through streets and damaging cars and basements. (It also killed more than 40 people across New York City.) But that hasn’t turned people away from the water.
As the climate warms, the city will have to reconfigure much of its urban fabric, particularly the 520 miles (837 kilometers) of shoreline. “It’s a mind-boggling scale,” says Ellis Calvin, a planner and data research manager at the independent nonprofit Regional Plan Association (RPA), as we stand at the water’s edge. By the middle of the century, the New York City Panel on Climate Change estimates, temperatures in the city could be hotter on average by 4 to 6 °F (about 2 to 3 °C), with several heat waves per summer. Sea levels could rise 11 to 21 inches (28 to 53 centimeters) by the 2050s and up to six feet (1.8 meters) by 2100—doubling the size and population of the 100-year-flood zone, the area that has a 1% annual chance of flooding. The borough with the most land affected by all this will be Queens.