With the Alaska Nanooks on their second consecutive week off, we dip into the archives for our hockey fix. I’m guessing this was the championship game of the 1936 Winter Carnival tournament. 1936 would have been the second annual winter carnival. Fairbanks won the game, although no score, or photog credit was given.
Tag Archives: UAF
Between 1930 and 2015, Fairbanks had a total of five Halloweens with less than an inch of snow on the ground. Counting this year, we have had five years since 2015 with less than an inch of snow on the ground. Currently, we have a dusting, and with 40F degrees forecast for Halloween Weekend, the odds are in favor of a brown Halloween for 2021.
Starting on Tuesday, the official average daily high temperature for Fairbanks dropped below the freezing mark. It does not rise above 32F until March 30.
October is American Archives Month:
1920’s travel along the narrow gauge rail of what was originally the Tanana Valley Railroad. By 1920, the TVRR had been bought out and this section renamed the Chatanika Branch. In 1923 it all became part of the Alaska Railroad.
Wildfires within Alaska burned less than half the usual acreage in 2020, which is not really a surprise with an unusually wet summer.
Fairbanks had its 12th warmest and 20th wettest summer in the past 90 years.
Anchorage saw its 23rd warmest and 28th wettest in the past 70 years.
Juneau had its 10th warmest and 15th wettest in the past 81 years.
The western coast of Alaska was just plain wet.
Bristol Bay had some very rough seas during the fishing season, but that didn’t keep them from setting a record year for sockeye salmon.
The Yukon River drainage had no salmon in 2020. No chums. No kings. Nada. The entire fishery was closed.
One bright spot was the amount of sea ice in the Chukchi Sea in August. It was the most we have seen in 15 years.
Denali National Park has already seen 6″ of the white stuff.
Fairbanks has already seen frost.
Luckily, we have not had a bad wildfire season in Alaska for 2021. We did have a fire flare up close to Fairbanks late last week, when smokejumpers, seen above, landed at UAF’s LARS location, where the herd of muskox can be seen roaming the hills. From the muskox field, the smokejumpers hiked the half mile to the fire’s location. That fire was quickly under control, and the firefighters went back to the Munson Creek fire soon after they were dispatched.
With just under 180,000 acres burned within the state so far this season, it puts us roughly equal with 2020 and within the lowest range of burned area since 2008. The Interior remains in a burn ban, but historically, 2/3 of acreage within a season has burned by July 15.
Figures,facts, graphics and video all from the Alaska Division of Forestry
The Yukon River mail run, leaving Eagle, Alaska around 1906. Currently, only media mail still travels this way within the state.
Muldrow Glacier in Denali National Park is surging:
In early March, pilot Chris Palm, who took the photo above, noticed something very different about Denali Park’s famed Muldrow Glacier. The normally smooth surface of the glacier was broken up by crevasses stretching across the width of Muldrow.
The long awaited surge had begun.
The 39 mile long, Muldrow Glacier last surged in 1957, so scientists were thrilled to study a natural phenomenon that has not occurred here in 64 years.
Surge-type glaciers are relatively rare, with approximately 1% of the glaciers world-wide being surge glaciers. Denali National Park has several, most of which get their start from the face of North America’s tallest peak.
As snow and ice builds up at the higher elevations of a glacier, meltwater is also building up underneath the glacier. This meltwater acts as a lubricant when the weight from above passes equilibrium. The glacier then surges downward at a rate of up to 100 times faster than normal. At some point, the meltwater trapped under the glacier will be released in an outburst flood. Once the water is reduced significantly, the glacier’s surge will slow and it will go back to a state of quiescent (non-surge) once again. Over time, the process repeats itself. Muldrow Glacier has a history of surging roughly every 50 years.
There are two GPS stations on the glacier to monitor its movement. There are also four time-lapse cameras facing different areas of the glacier, including one at the terminus to monitor the glacier’s “bulldozing action”. Another is looking over the McKinley River in order to capture images of the outburst flood. The Alaska Earthquake Center also has a seismic monitoring station, and a sound station has also been installed in an attempt to capture the grinding sound of the surging glacier.
In 1957, most accounts have the surge starting in May, 1956 on Traleika Glacier, which is the main tributary of Muldrow. Muldrow Glacier would advance over 4 miles before the surge ended in September of 1957. Approximately 3.3 cubic kilometers of ice was redistributed from the upper reaches of the glacier to its toe. At the upper levels, the ice thickness had dropped as much as 170 meters, but the toe rose to a 200 foot tall ice wall.
Currently, the Muldrow Glacier is moving between 10 to 20 meters per day, and is only 800 meters short of the 1957 terminus. At the current rate of surge, Muldrow will reach the 1957 distance in June.
All images, photos and maps are courtesy of the NPS; Sources include: NPS – Denali NP&P, Alaska Department of Natural Resources, University of Alaska – Fairbanks
In 1963, a young, male bowhead whale was harvested by Native Whalers in Utqiaġvik. The skeleton of the 43′ whale was eventually offered to the University of Alaska – Fairbanks, and it has been in the collection of the Museum of the North ever since. Only the skull has been put on display.
That is about to change, as the Museum is currently putting together the entire skeleton, and will display it from the lobby ceiling once it is complete.
The above video from the UAF Museum of the North, details some repair that had to be done to the ribs of the bowhead whale.