Where Did the Hurricane Energy Go?

The 2026 Atlantic hurricane season is incredibly rare and historic, but for a surprising reason: it is tracking at a record-breaking low for activity. Despite the destructive flooding along the East Coast, not a single hurricane has formed in the Atlantic basin. While the coast is currently being battered by a powerful nor’easter, the system is an extra-tropical winter-style storm, not a tropical hurricane.

September 23, 2026

The Jersey Shore experiment

A powerful and exceptionally persistent September nor’easter is affecting the Jersey Shore, bringing coastal flooding, dangerous surf, strong northeast winds, and significant beach erosion. The National Weather Service has extended the Coastal Flood Warning for Ocean, Atlantic, Cape May, and southeastern Burlington counties through Sunday, September 27. The warning calls for one to two feet of inundation above ground level in vulnerable low-lying areas near shorelines and tidal waterways, with widespread roadway flooding possible.

This is shaping up to be one of the most persistent nor’easters in modern history, with significant coastal impacts continuing for days rather than hours. The prolonged onshore winds are repeatedly pushing water toward the coast, while high surf and wave action continue to pound beaches and barrier islands.

The combination of persistent winds, elevated water levels, astronomical tides, and repeated wave attack makes this much more than a single coastal storm event. It is an extended assault on an already vulnerable coastline.

Along portions of the coast, the National Weather Service is also warning of high surf, with breaking waves reaching approximately nine feet in the surf zone.

The timing is important. The storm is occurring during the full-moon period, when astronomical tides can increase the baseline water level and make coastal flooding more consequential.

So here is the experiment: watch and determine the cost.

September 29, 2026

The late-September 2026 nor’easter turned atmospheric and oceanic energy into a massive economic event.

$10–13 BILLION in estimated damage and economic losses.

Flooding.
Beach and dune erosion.
Downed trees.
Power outages.
Infrastructure damage.
Transportation disruption.

The storm demonstrates a simple connection:

STORM ENERGY → FLOODING + EROSION + WIND → DAMAGE → ECONOMIC LOSS

Climate energy does not remain an abstract number measured in joules.

It reaches us through the places where we live, the infrastructure we depend upon, and the economic systems that connect us.

The Jersey Shore: Erosion, Flooding and Infrastructure Damage

The most concentrated physical damage occurred along exposed coastal communities.

Atlantic City

Atlantic City experienced some of its most severe beach erosion since Superstorm Sandy in 2012. A particularly hard-hit area extended for approximately a half-mile north of Steel Pier.

The storm carved deeply into the dunes, leaving steep sand escarpments and exposing previously buried structures. Atlantic City Beach Patrol officials reported that roughly half of the dunes remained in the affected area after the storm.

This is more than a cosmetic change to the beach. Dunes function as part of the coastal defense system. Removing large quantities of sand reduces the physical buffer between ocean waves and developed areas.

Brigantine

Brigantine also suffered extensive beach and dune erosion. City officials estimated that hundreds of feet of beach were washed away, while approximately 30 feet of dunes were lost in one particularly vulnerable area. Officials said the damage could amount to tens of millions of dollars.

The storm also damaged the city’s promenade. A newly installed beach-access ramp was torn from its foundation and carried approximately 30 blocks down the beach before being recovered. Sections of promenade railing were also damaged.

Mayor Vince Sera described the storm as producing exceptionally powerful ocean conditions, while city officials emphasized that the promenade and seawall helped protect homes and infrastructure from even greater damage.

Repeated Tidal Flooding

The storm’s slow movement and persistent onshore winds produced flooding over multiple high-tide cycles.

In Sea Bright, New Jersey, for example, successive tides repeatedly flooded neighborhoods rather than producing a single isolated flooding event. More than four inches of rain also fell in portions of New Jersey, adding freshwater runoff to the coastal flooding problem.

The combination of heavy rainfall + elevated ocean water + high tides + strong onshore winds created a compound flooding event.