Alaska and Northwestern Canada quarterly climate impacts and outlook: December 2017
Weather and climate highlights and impacts, September to November 2017; Climate outlook January 2018 to March 2018
Map of Alaska and North-West Canada showing weather and climate highlights and impacts between September and November 2017.
- Utqiaġvik (Barrow): US$10 million damage due to coastal erosion from an Arctic storm on September 28th-30th
- Beaufort/Chukchi Seas: Near record low autumn sea ice extent
- Shishmaref: Severe erosion from November 11th-12th storm caused the city and tribe for Shishmaref to issue disaster declarations to the State Emergency Operation Center, Alaska
- Fairbanks: October 9th-10th 39.1mm (1.54”) of precipitation is the record 24 hour precipitation amount for the month of October
- Old Crow: 5th warmest October on record with an average temp of -5.2°C (22.6 °F)
- Dawson: Fifth wettest September-November on record; 130 mm (5.1”)
- St. Paul: Warmest November since 1926 with an average temperature of 4.1°C (39.4°F)
- Anchorage: September 13th minimum temperature of 13°C (55°F) is the highest minimum recorded for the month of September
- Hyder: September 5th maximum temperature 29°C (84°F) just one degree Fahrenheit shy of the monthly record for the state
- BC/Yukon: An Arctic outbreak began on November 2nd, which set more than 30 daily low temperature records
- Fort St. John: Record breaking snowfall of 55 cm (2.2”) in Fort St-John on October 24th-25th
Temperature and precipitation, September 2017 to November 2017
Much of mainland Alaska, northern Yukon Territory and large swath of the western Northwest Territories (NWT) was significantly warmer than average for autumn 2017. Most of the remainder of the region had, on average, near normal temperatures, except for a small swath from the central Yukon Territory south and eastward into the northern Alaska Panhandle and northern British Columbia, where temperatures averaged significantly below normal. Total precipitation was significantly above average over much of northern and western sections and northeast British Columbia, but below normal along the Gulf of Alaska coast into northwest British Columbia and parts of the Yukon and NWT.
La Niña likely to make a return this winter
A typical La Niña winter pattern features high pressure across the Bering Sea that reduces the numbers of storms tracking into the region and is favorable for the development of a colder than normal airmass across northwest North America. This is in contrast to El Niño, when a storm track into the northeast Pacific and Gulf of Alaska is favored, bringing milder air into northwest North America, and near the coast increased precipitation. La Niña sometimes features large swings in the week to week weather pattern, which again is in contrast to El Niño winters, where the weather pattern is often very stable for long stretches of time.
Under a weak La Niña climate pattern, most of NW Canada may experience colder than average temperatures, while the South Coast of BC may experience above-average precipitation.
Impact of weak to moderate La Niña to Pacific NW and Alaska
These graphics show departures of temperature (left) and precipitation (right) from the long term averages for January through March during eight winters between 1979 and 2016 when there was a weak to moderate La Niña. The left figure shows that during recent La Niña winters, the majority of Alaska and the west coast of British-Columbia had colder than averaged conditions (blue), while the region east of the Mackenzie River experienced warmer than averaged conditions (red). The right figure shows that during recent La Niña winters, Western Alaska had drier than averaged conditions (brown), while most of the remainder of the region had moister than normal conditions (green).
These graphics show departures from the long term averages for January through March during eight winters between 1979 and 2016 when there was a weak to moderate La Niña. Most of North America west of the MacKenzie River finished up cooler than average during late winter season. Western Alaska has averaged drier than average during recent La Niña, while most of the remainder of the region has tilted toward higher precipitation. Even in these eight winters (1984, 1985, 1996, 1999, 2001, 2008, 2011 and 2012), there is significant variation in most areas.
Sharp warming in air temperature at Utqiaġvik flagged as artificial change
Air temperature at Utqiaġvik (Barrow) increased by up to 7.8°F (4.3 °C) between 1979-1999 and 2000-2017 for the months of October-December. This warming was large enough to trigger an algorithm designed to detect artificial changes in a station’s instrumentation or environment and disqualify the entire 2017 air temperature measurements. The warming was a result of decreasing sea ice area in the Chukchi and Beaufort Seas, exposing more relatively warm Arctic water to the atmosphere than when sea ice in the region is large. The discarded Utqiaġvik data is progressively restored and incorporated in the National Centers for Environmental Information Alaskan temperature to reflect the climate change that changed the environment. Additional information can be found here.
Sea ice conditions at the end of November 2017 in the Beaufort and Chukchi Seas
Sea ice continued to recede away from Alaska during September, with no ice within 100 miles (160km) of Alaska at the end of the month. Ice grew only slowly during October and November. This lack of ice allowed for several late season coastal flood and severe erosion events to impact some western Alaska communities. The Beaufort was largely iced over mid-November, but open water stubbornly persisted in the Chukchi Sea. By the end of November there was still open water far to the northwest of Utqiaġvik. The combined Chukchi and Bering sea ice extent was only half of the 1981-2010 average and the lowest on record in the satellite era (since 1978) (data from National Snow and Ice Data Center).
Following a greater than normal ice melt for the Beaufort Sea areas this past summer, the onset of freeze up was significantly delayed. Generally speaking ice formation over the area was 3-4 weeks later than normal. However by mid-December, the area was almost entirely covered with ice (no significant departure as shown on the map). With the delayed ice formation, ice thicknesses were also thinner than normal. At the end of the melt season, this year ranked as the 7th lowest minimum ice extent in the Beaufort Sea area.
Map showing the departure from normal of ice concentration for the Beaufort Sea for November 27th, 2017. The map shows that the majority of the Beaufort Sea areas have the normal concentration for that day (white on the map). Only a small area north-west of the Alaska coastline shows a reduction of 4-7 tenths of ice.
Temperature and precipitation outlook: January to March 2018
The calibrated categorical forecasts from the 100 plus member North American Multi-Model for January-March 2018 show increased chances for significantly below normal temperatures over northern British Columbia, the central and southern Yukon Territory, westernmost NWT and adjacent areas on southeast Alaska mainland and Panhandle. The only area with increased chances for significantly above normal temperatures are small areas in coastal western Alaska, which is consistent with the expectations during a La Niña winter.
Precipitation forecasts show a wet tilt across northwest Alaska and the western Interior. In contrast, from Kodiak Island eastward into the northern Alaskan Panhandle, extreme northwest British Columbia and parts of the Yukon and southwest NWT there are slightly increased odds for significantly below normal precipitation.
The map shows the forecast for the probability of a departure from normal temperatures for January-March 2018. On the map, northern British Columbia, the central and southern Yukon Territory, westernmost NWT, and adjacent areas on southeast Alaska mainland and Panhandle are expected to have a 40% or less chance of below normal temperatures for the period. Small areas in coastal western Alaska, on the other hand, have up to 50% chance of above normal temperatures for the period.
The map shows the forecast for the probability of a departure from normal precipitation for January-March 2018. On the map, northwest Alaska and the western interior have a 40% chance or less of being moister than normal for the period. In contrast, the region from Kodiak Island eastward into the northern Alaskan Panhandle, the extreme northwest British Columbia, and parts of the Yukon and southwest NWT have a 40% chance or less of below normal precipitation.
Content and graphics prepared in partnership with the Western Region Climate Center, NOAA National Weather Service Alaska Region, and Environment and Climate Change Canada.
Alaska Region Partners: Western Region Climate Center, Alaska Climate Research Center, Alaska Climate Science Center, Cryosphere Today, NOAA / NWS Weather Forecast Offices, NOAA / NESDIS / NCEI, Scenarios Network for Alaska + Arctic Planning.
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Western Canada partner:
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