Alaska's Villages Flooded. The Rescue Was Only the Beginning

In October 2025, the remnants of Typhoon Halong reached western Alaska. The storm had formed in the western Pacific, tracked north, and carried its moisture into the Bering Sea region. What arrived was not a typhoon anymore. It was a massive low-pressure system that brought record rainfall and storm surge to communities that sit on some of the most remote coastline in the United States.

The villages of western Alaska are not connected by roads. They sit along rivers and coastlines, accessible only by air or water. When the flooding hit, there was no driving to safety. There was only waiting for rescue or moving to higher ground that, in many places, did not exist.

The Storm Arrives

Typhoon Halong formed in the western Pacific and followed a track that carried it north toward the Aleutian Islands and the Bering Sea. By the time it reached Alaska, the system had lost its tropical characteristics but retained enormous amounts of moisture. NOAA satellites tracked the remnants as they merged with weather systems already in the region.

The result was rainfall that exceeded anything the affected communities had experienced in recorded history. Rivers rose. Low-lying villages flooded. Storm surge pushed seawater inland along the coast. The combination of river flooding and coastal surge trapped communities between rising water on all sides.

Rescue at Kipnuk

Kipnuk, a Yup’ik village of roughly 700 people on the western Alaska coast, was among the hardest hit. The village sits on low ground near the Kuskokwim River delta. When the water rose, homes flooded. Essential infrastructure was submerged.

U.S. Coast Guard aircrews launched rescue missions from their stations in Alaska. The footage captured by Coast Guard cameras shows what rescue looks like in a place where the nearest road is hundreds of miles away. Helicopters flew over landscapes where the boundary between land and water had disappeared. Rescue swimmers deployed to reach people stranded by the rising flood.

The rescues at Kipnuk were the visible, urgent phase of the response. But as the video’s title says, the rescue was only the beginning.

Operation Halong Response

The Alaska National Guard activated Operation Halong Response. Military aircraft flew from Joint Base Elmendorf-Richardson near Anchorage to the affected region. The mission was evacuation: getting displaced residents out of flooded villages and into safe shelter.

Ninety-six displaced Alaskans were evacuated to JBER. The evacuees arrived with what they could carry. Behind them, their homes sat in water. The footage from DVIDS shows the evacuation process: families boarding military aircraft, arriving at the base, and being processed into temporary housing.

The scale of the operation reflected the geography. Western Alaska is not a place where you can send a convoy of trucks. Every person evacuated, every piece of equipment delivered, and every supply shipment had to move by air. The logistics of disaster response in remote Alaska are fundamentally different from anywhere else in the United States.

The Recovery

After the water receded, the work shifted from rescue to recovery. Alaska National Guard crews returned to the affected villages to begin cleanup. The footage shows what flood recovery looks like in a place where replacement materials cannot be driven in: damaged homes, debris scattered across village sites, and crews working with limited equipment to restore basic services.

The recovery was not measured in days. It was measured in weeks. Each flight into a village carried supplies and personnel. Each flight out carried debris and damage assessments. The remoteness that defines life in western Alaska became the defining constraint of the recovery effort.

A Pattern of Vulnerability

Western Alaska’s villages have faced flooding before. The combination of low-lying terrain, proximity to rivers and coastline, and exposure to storms from the Bering Sea makes these communities vulnerable to exactly the kind of event Typhoon Halong’s remnants produced.

Climate change is compounding the problem. Reduced sea ice means less protection from storm surge. Thawing permafrost destabilizes the ground that villages are built on. Rising temperatures increase the moisture content of storms that reach the region. The 2025 flooding was record-setting, but the conditions that produced it are becoming more common.

The footage from this disaster tells two stories. The first is the rescue: helicopters, swimmers, evacuations, the urgent work of getting people to safety. The second is the recovery: the slow, logistically constrained process of rebuilding communities that are hundreds of miles from the nearest hardware store, the nearest road, the nearest anything.

The rescue made the news. The recovery did not. But for the people of Kipnuk and the other affected villages, the recovery is the part that determined whether they could go home.