Flooding in the Tanana Valley during mid-August 1967 was the most widespread, damaging flood of record in Alaska. Six deaths were attributed to the flooding. Total flood damage was estimated in excess of $85 million (1967 dollars); both Fairbanks and Nenana were declared national disaster areas. The flooding resulted from torrential rains, in part from moisture from ex-typhoon Holly, following what had already been a wet summer. Rainfall amounts over a large area were far more than ever seen before or since. In many places, rainfall totals for August were one half to three-quarters of the normal ANNUAL precipitation. More than 12,000 people were evacuated during the flooding. The entire city of Fairbanks was flooded, and the Richardson Highway, the only road connection at the time to points south was cut off due to highway washouts near Salcha. Hundreds of people were flown to Anchorage and thousands more took shelter at the University of Alaska's hilltop refuge.

Following the flood, recovery efforts were frantic in an effort to rebuild and repair before sub-freezing weather returned. The impacts of this flood are felt to this day: residents of the community of Minto, which had been subject to frequent floods even before to this event, abandoned their entire community relocated and moved to a less flood prone area nearly 20 miles to the north.

As a result of this flood, a number of river and precipitation gages were installed in the Chena River basin and the Moose Creek Dam flood control project near North Pole was built to divert water from the Chena River when needed and so reduce future flood threats to Fairbanks, Alaska’s second largest city.

Photos of Fairbanks, Alaska, showing the inundation of the city, from "Floods of August 1967 in East-Central Alaska.” USGS 1972

Additional Images available from the University of Alaska 

April and early May 2013 were the coldest in decades in Interior Alaska. As a result, the winter snowpack in the Yukon River basin, which was generally near normal at the start of spring, remained in place weeks later than normal, and river ice remained solid. Flooding on the Yukon River in Alaska occurred at Eagle on May 17, when a short-lived ice jam backed up water into several homes. The community of Circle City flooded on the morning of May 19, when an ice jam developed just below town. Almost every building in town had some water damage. Fortunately, the jam broken quickly and the water receded. A major ice jam formed above Fort Yukon, but rather than releasing all at once, the jam was gradually eroded and as a result there was only minor flooding. 

By far the worst flooding occurred at the middle Yukon community of Galena. An ice jam formed May 26 at Bishop Rock, 18 miles downriver from Galena. Ice backed up more than 40 miles behind the jam before the jam released on May 29. As the water rose at Galena on the 26th, evacuations began, and by the 28th most residents were evacuated by air. Those remaining were forced to camp at the levee-protected airport without electricity or waste water sanitation. Some buildings in the old section of town were lifted off their foundations and floated away. The vast majority of buildings sustained flood damage and many were uninhabitable, and most of the old town section will not be rebuilt. A federal disaster declaration was issued in late June. 

Recovery was slowed by the extent of infrastructure damage: even the road to the dump washed out and had to be rerouted. Because the Galena school was housing some residents as well as recovery personal who were working over the summer, school was 3 weeks late in resuming in the autumn. The combined costs to the state and federal governments for relief and recovery efforts, as of early October 2013 were estimated to exceed $80 million. Fortunately, there were no deaths or serious injuries.

May 28, 2003 looking north, showing the ice-clogged Yukon River. The dike-protected airport is clearly visible

Two separate periods of prolonged heavy rain during mid and late August 1994 in the Koyukuk River Basin produced severe flooding in middle sections of the river. Rainfall amounts during the second half of August in the region were generally 50-75% of the normal annual total. All 200+ residents evacuated from the neighboring communities of Allakaket and Alatna, where almost every building was damaged or destroyed by water that in some places was 10 feet deep. Farther downriver at Hughes, damage was less complete but still substantial. The area was declared a national disaster in September 1994. Because the flooding occurred so late in the summer, many residents were forced to spend the winter in other communities. Rebuilding took place primarily in the summer of 1995. Total damage exceeded of $15 million. Total cost including repair, relocation, evacuation and mitigation exceeded $70 million (1995 dollars). Ther were no deaths or serious injuries.
 

Photo courtesy of Alaska Division of Community & Regional Affairs

 

Persistent warm, moist southerly flow during mid and late September 1995 and the resulting orographically focused rains produced severe flooding across parts of south central Alaska. Some low elevation locations received in excess of 20 inches of rain in a week and twice that amount likely fell at some higher elevations. Unusually high freezing levels for so late in the season allowed for significant high elevation glacier and snowmelt which contributed to the very high water levels. Peak water volumes on the Eagle and Knik Rivers north of Anchorage were estimated to have reached a once in 500 years level. Damage was especially severe along the Kenai River and in Seward and Girdwood. The lower Kenai River on the Kenai Peninsula crested September 24 and remained above flood stage for moer than 10 days. Impacts of the flooding includes damage to cabins, permanent homes, sewage treatment facilities, roads, trails, bridges, power transmission lines, airports and railroad facilities. Fast currents caused significant bank erosion, channel shifting, and damage to dikes and levees. Total damage was estimated at over $10 million and the President declared it a Federal Disaster Area area October 1995. There were no deaths or serious injuries.

The impacts of this flood are still felt today, with bankside restoration undertaken to mitigate future flooding. A much improved network of river and rain gauges, including some at higher elevations, was installed in the aftermath of this flood to provide better monitoring and improved forecasts.

National Weather Service Flood Report: South Central Alaska Floods Sep 19- October 2, 1995

A unique flooding issue in Alaska involves lakes that form behind glaciers. Many of Alaska’s glaciers flow across the mouths of adjoining valleys and cause lakes to form behind the ice. These ice dams are subject to repeated failure and as the volume of the lake enters into the downstream rivers, it can cause extreme and sudden rises in water level and may result in minor to major flooding.

One location famous for destructive flood events is on the Knik River near Palmer. From 1918-1963, Lake George formed behind the Knik glacier and annually emptied in July or August and then refilled. At the time, Lake George was the largest glacier dammed lake in Alaska and the regular release turned into such a spectacle that the area was designated as a Natural Landmark by the National Park Service. Something changed in the mid 1960s and after 1966, the lake stopped forming (Post and Mayo, 1971).

Another dramatic glacier dam release occurred from a lake on the Skilak Glacier above Skilak Lake on the Kenai River in 1969. The volume of the release was relatively small, causing less than a foot rise on Skilak Lake, but the timing of the release, in January, caused a breakup of the river ice which moved downstream and jammed the river causing flooded roads, homes and businesses in the middle of the winter and then freezing in place. Glacier dammed lakes on the Snow and Skilak glaciers release regularly on the Kenai River, typically every 2 years and cause a 2-4 foot rise on the river, which can result in flooding depending on the river level at the time of the release.

 A final example of glacier dammed lakes is the one formed by the Hubbard Glacier in Russell Fiord. Hubbard glacier (upper left of the map) has threatened to close the gap entirely, preventing Russell Fiord from flowing into the Gulf of Alaska through Disenchantment Bay. In 2002, the glacier actually closed the gap sufficiently that the inflows to Russell Fiord exceeded the outflows through the restricted space by a considerable margin, raising the level of Russell Lake by 61 feet above sea level over a 2½ month period. When the lake started to erode through the glacial blockage, the outflow increased significantly, eventually releasing about 0.9 cubic miles of water. The peak outflow exceeded the peak historic flow of the Mississippi River at Baton Rouge by about 30%. The Hubbard Glacier continues to surge and eventually is likely to close off the gap entirely. Several federal agencies continue to monitor Hubbard Glacier because if the gap does close, the resulting lake could rise to 130 ft above sea level at which point it would spill into the Situk River near Yakutat which is a prized salmon and steelhead stream.

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