Southeast Alaska Extreme Snowfall

Historic snowfall to end 2025

Northern Southeast Alaska experience historic snowfall the last days of December as persistent moist southwest flow aloft rode up and over an entrenched Arctic airmass near the ground. Between December 27 and December 31, near sea level, three to seven feet of snow fell from Juneau northward. There were only a few short breaks in the snow between when the snow started on the morning on December 27 and ended later on New Year’s Eve.

How much snow fell?

Because of the long duration and excessive amounts, not all observations are complete or available yet, but here’s what’s been reported so far. These are a mix of official and unofficial reports but all appear plausible. I’ll update this post as additional information comes online.

Juneau area snowfall

• Mile 26 Glacier Highway: 52 inches

• Lena Point: 49.2 inches

• Airport: 49.0 inches (the long term climate site)

• Mendenhall valley (NWS Forecast Office): 43.2 inches

• Snettisham Power Plant: 26.0 inches (significant rain one day)

Some boats in the Juneau Harbor sunk due to the weight of the snow and there were a number of mostly short-lived power outages. News reports on the storm and impacts from KTOO in and around Juneau here and the Juneau Independent, here.

An unoccupied vehicle blocks an unplowed street in downtown Juneau on the night of Tuesday, Dec. 30, 2025. (Mark Sabbatini / Juneau Independent)

Other snow stats from Juneau airport include

• highest 5-day total on record, 49.0 inches, previous record 45.9 inches April 1-5, 1963.

• highest snow depth 50 inches on December 31, previous record 41 inches Feb 24, 1949

• highest December snowfall, 82.0 inches. This is the second highest monthly snow of record, only higher was February 1965 with 86.3 inches. However, this is well below highest 31-day snowfall in Juneau weather history, which is 98.9 inches January 27-February 26, 1965.

Haines area snowfall

• 7 miles southeast: 79 inches

• 5 miles south-southeast: 77 inches

• 1 mile northwest: 61 inches

• Haines Highway Customs station: 27.5 inches there precipitation totals were much lower here, probably due to mountains to the southwest intercepting some of the moisture.

Other reports:

• Gustavus: 55.2 inches

• Elvin Cove: 41 inches

• Yakutat: 30.9 inches

Central and southern Southeast Alaska also received snow at the start of the storm but then temperatures warmed aloft (and eventually at the surface) to allow some or most of the precipitation near sea level to fall as rain. Snowfall totals reported before the switch to rain:

• Hoonah: 36 inches

• Hyder: 33 inches

• Petersburg: 15 inches

• Kake 17 miles west: 13 inches

• Ketchikan 10 miles north: 8.1 inches

The water equivalent of the snow over the five days was high, though not extreme. At the NWS Juneau forecast office, the December 27-31 total precipitation was 4.80 inches.¹ Just in the past 25 years there have been five other 5-day intervals in December that had more precipitation.

The weather set-up

The excessive snowfall was the result of the confluence of high pressure and an Arctic airmass over the Yukon Territory and northwest British Columbia and very moist southwest flow aloft. As the Arctic area was locked in place, there was a continuous replenishing of the cold air into northern Southeast Alaska. A surface analysis from the NWS Ocean Precipitation center shows the set-up mid-way through the storm. Sprawling high pressure extended from the central Brooks Range southeastward across the Yukon Territory and broad low pressure was centered in the western Gulf of Alaska. The surface boundary of the cold air (shown as a stationary front) is just south of Juneau (Fig. 1).

Fig. 1 NWS Ocean Prediction sea level pressure and surface frontal analysis valid 3pm AKST December 29, 2025.

While this was not a classic atmosphere river (AR) set-up for Southeast Alaska, there was a wide belt of substantial subtropical moisture feeding into Southeast Alaska (Fig. 2), even though the core of the AR was farther south into Haida Gwaii, BC.

Fig. 2 U.S. Global Forecast System 700 hPa heights (contours) and integrated vapor transport (colors) for at 3am AKST December 28, 2025. Image courtesy polarwx.com

We can put get an idea of these two factors together by combing the mid-atmospheric flow pattern with the low level temperatures (Fig. 3). Note the NCEP/NCAR reanalysis (the only reanalysis available for the event as I write) is too coarse to do justice to the exactly where low level cold air was entrenched, but it illustrates the concept. Very warm air was over the southeast Gulf of Alaska and into southern Southeast, but being less dense than the Arctic air, it was forced up over top of the cold air, and the result was five days of snow.

Fig. 3 Average 700 hPa (roughly 10,000 feet MSL) heights and 850 hPa temperatures (roughly 4500 feet MSL) for December 28 and 29, 2025. Data courtesy NOAA/Physical Sciences Laboratory.

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Data sources:

Most of the snowfall amount reports come from Local Storm Reports issued by NWS Juneau and are easily retrievable through the Iowa Environmental Mesonet, here.

NWS and cooperative observations from NWS Juneau climate webages, here, and xmACIS, here.

1. Precipitation from the automated weather station at Juneau airport during the storm was unrealistically low.