In this issue
- Weather and climate highlights and impacts for March–May 2019
- Climate Outlook for July–September 2019
Temperature and precipitation, March–May 2019
March to May 2019 temperature averages and anomalies
March to May 2019 precipitation averages and anomalies
A very warm month of March: the influence of the atmosphere, oceans and sea ice
March 2019 was exceptionally mild over nearly all of Alaska and northwest Canada, with many locations in mainland Alaska, Yukon and western NT recording the mildest March on record by a wide margin. At Inuvik, NT, the average March temperature was a stunning 14.4 °C (25.9 °F) above the 1981-2010 normal. In Alaska, the Deadhorse Airport at Prudhoe Bay averaged 23.8 °F (13.2°C) above normal, and Fairbanks had the warmest March in 115 years of climate records.
So why was it so remarkably mild over such a large area? Three main factors were involved:
- A persistent high pressure system over the region
- Record-low sea ice extent
- Warm ocean temperatures.
These factors, explained below, illustrate the cumulative importance of the atmosphere, oceans and sea ice to the regional climate.
First, a massive high pressure at mid-levels (500 mb) of the atmosphere was anchored most of the month over eastern Alaska and northwest Canada. High-pressure systems are typically associated with clear skies and calm weather. The absence of clouds in the atmosphere to block incoming solar radiation causes surface air temperature to rise during the day. In March 2019, the persistent high-pressure system was one of the strongest at this time of year in the region since 1949, as shown by the red and orange areas on the figure below. The associated warm air, combined with longer daylight, sunshine and accelerated snowmelt gave a major boost to temperatures.
Secondly, sea ice extent in the Bering Sea was the lowest on record in March 2019. This low sea ice extent was associated with frequent areas of exposed water in the southern Chukchi Sea. The mere presence of water instead of the normal snow covered sea ice is a significant source of heat transfer from the ocean surface to the atmosphere as greater warming occurs in ice-free regions. The figure on the top-right illustrated open water on the Bering Sea on March 13, 2019.
Thirdly, south of the sea ice in the Bering Sea, ocean surface temperatures were well above normal, as they have been for much of the past several years. These warm ocean surface temperatures provided an additional source of ocean heat, which in turn, contributed to the warming of surface air temperatures in southwest Alaska.
Low precipitation, drought, and impacts on water levels
Most of northwestern Canada and Alaska had low winter 2019 snowfall accumulations, with some areas seeing some of their driest winter on record. This is a continuation of low precipitation and dry conditions in the region. In fact, parts of southeast Alaska, northern BC, and southern Yukon have been experiencing drought conditions for the last two years as a result of low precipitation amounts (see Figure below).
As a consequence of low precipitation amounts, most Yukon, NT, and Alaska rivers were running below average in May 2019. Along the Yukon River near Whitehorse, these low water levels had an unexpected consequence: historical objects and structures such as old rusty nails, wooden logs and pieces of sternwheelers that are typically well hidden under water or ice have been uncovered. These artifacts provide a piece of history along the Yukon River.
However, despite low precipitation and low river flows, near record-breaking March 2019 temperatures produced rapid spring snowmelt. This led to localized flooding in some Whitehorse neighborhoods as the rapid melt overwhelmed the storm drains in late March.
Sea ice conditions at the end of May and beginning of June 2019 in the Beaufort and Chukchi Seas
Sea ice extent in the Bering Sea was at a record low (since 1979) in March 2019, which is even lower than in 2018. Early April 2019 saw some recovery in extent, but the new ice was very thin and quickly melted out when the weather pattern changed. Sea ice in the southern Chukchi Sea was fractured and mobile in March and early April 2019, with open water frequently appearing in Kotzebue Sound. Seasonal melt began in earnest in mid-April 2019 and rapidly expanded northward, with total sea ice extent at record low levels in mid and late May 2019. In the Beaufort Sea, sea ice melt beyond the shorefast ice was very rapid and 6 to 8 weeks ahead of 2018 melt. By the first days of June 2019, the only remaining sea ice in the Bering Sea was in the western Gulf of Anadyr. At the same time, the Chukchi Sea open water was found northwest of Utqiaġvik at 72° N, and only a thin band of sea ice northeast of Point Barrow separated open water from the Chukchi and Beaufort Seas.
The ice extent in the Beaufort Sea was stable for the latter part of winter and into the first part of spring. However, after mid-April 2019, signs of breakup began to appear in the southeastern part of the Beaufort Sea, just north of the Tuktoyaktuk Peninsula, NT. By the end of May/early June 2019, the breakup was well underway in most of Amundsen Gulf, the southeastern Beaufort Sea area, and the region near Point Barrow. In fact, the open water along parts of the northern Alaskan coast was up to six weeks to two months earlier than normal. In the meantime, the coastal fast ice was fracturing two weeks earlier than normal. By the end of May 2019, significant open water areas and looser than normal ice conditions from the Amundsen Gulf to the north coast of Alaska represented ice conditions up to two months earlier than normal.
Outlooks for July–September 2019
A combined Canada-USA climate forecast model is used to provide temperature and precipitation outlook for July-September 2019.
The temperature outlook for July through September 2019 shows that Alaska and northwest Canada have a 40-95% chance of above average temperature (orange-red colors), with highest probabilities found in the southwestern parts Alaska (including the Aleutian Islands), southern Yukon, and northern BC. A small area in northwestern NT along the Beaufort Sea including Banks Island and the western portion of Victoria Island, as well as an isolated pocket in northern Alaska, have a 40-50 % chance of below average temperature (blue areas).
The precipitation outlook for July through September 2019 shows that the majority of Alaska, northern BC, southern and western Yukon, along with the regions east and south of Great Bear Lake, NT, have a 40-50% chance of above normal precipitation (green areas). The majority of the NT, and small isolated pockets in western Alaska and northern Yukon have a 40-50% likelihood of below normal precipitation (brown areas).
Content and graphics prepared in partnership with the Alaska Center for Climate Assessment and Policy (ACCAP) and Environment and Climate Change Canada (ECCC).
Alaska Region Partners: Alaska Climate Research Center, Alaska Climate Science Center, National Snow and Ice Data Center (NSIDC), NOAA / NWS Weather Forecast Offices, NOAA National Weather Service Alaska Region, NOAA / NESDIS / NCEI, Scenarios Network for Alaska + Arctic Planning.