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EDITORIAL: With ranked choice voting, does Alaska still need primaries?

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EDITORIAL: With ranked choice voting, does Alaska still need primaries?


Even by the adjusted standards of a non-general election, Alaska voters’ participation in last Tuesday’s primary was anemic. Several factors were at play, of course: Other than the high-profile U.S. House race between Rep. Mary Peltola, Nick Begich III and Lt. Gov. Nancy Dahlstrom, there were few major draws on the ballot — and even the House race lacked the high drama of 2022′s special primary, where dozens of candidates were whittled to just four, or its general election, where Alaskans selected a candidate not named Don Young to Alaska’s sole U.S. House seat for the first time in almost 50 years.

Most of all, though, the biggest contributor to the lackluster primary election turnout was likely its lack of serious consequences. In selecting a better method to elect candidates — ranked choice voting — Alaska has unintentionally removed most of the stakes and necessity of contests prior to the November general election.

Under the state’s open primary system, instituted by the same ballot measure that gave us RCV, Alaska voters select the candidate they like best in the primary, similar to the old system (but with all candidates on the same ballot), and the top four vote-getters in each race move on to the general election. But nearly all races except statewide ones have fewer than four candidates anyway, so the practical impact of the primary is nil. To be sure, there were a few races where the primary had a winnowing effect — in Eagle River’s Senate seat, for instance, former Rep. Sharon Jackson was the red-lantern finisher among five candidates and was thus knocked out. Similarly, in a wide-open race for House District 36 in the rural Interior, Libertarian candidate James Fields came in fifth and won’t be on the November ballot. And in the aforementioned U.S. House race, eight also-rans who cumulatively secured just more than 2% of the vote were eliminated. But those were the only races that were affected by the primary — a tiny fraction of the 51 total races on Alaska ballots.

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Given the lack of paring-down in nearly all races, the principal utility that Alaska’s primary election has at this point is as a massive free poll for candidates and (if they have them) the parties that support them, giving them a sense of the state of the race three months before it’s actually contested. But the reality is that the data provided isn’t altogether predictive of future election returns — primary voters tend to be more motivated and more partisan than general election voters, so their preferences may not line up well with how things will go when the seats are decided. Other voters will be motivated to turn out in the general election by the presidential contest. And as RCV lets us rank all of the candidates who emerge, there’s less turnout incentive for primaries — even if a screwball or two ends up among the field, it’s a problem easily remedied by ranking other candidates higher. Sure, it’s interesting to see how people feel about the candidates in the race a few months out, but does that justify the expense of an entire election? If campaigns and parties want that information, it would make more sense for them to pay for polls rather than Alaskans doing the work (and shelling out public money to cover the cost) for them. Indeed, in some races — most notably the U.S. House race — we’ve seen candidates drop out in order to elevate a single candidate from one party. If the parties find utility here, we should be willing to ask ourselves: Should Alaskans fund an election just to help the parties get organized? The parties should fund and conduct that activity themselves if it’s useful for them.

There are a few edge cases where primaries would still have clear usefulness to Alaska voters — for instance, if candidate numbers skyrocketed to the point that ballots in November became unwieldy (say, if many races turned into the free-for-all of the 2022 U.S. House special primary), though that hardly seems likely. Even if six or seven candidates were on the general election ballot, ranking the top four would still easily decide elections, and it’s hard to imagine any race outcomes changing. Another low-likelihood scenario would be if bad actors registered candidates with similar names to a legitimate candidate in an attempt to confuse voters — but that’s a scenario that the status quo (or, for that matter, the old voting system) doesn’t guard against, either.

Alaska’s short history with ranked choice voting has so far been a strong success, giving candidates an incentive to consider the preferences of all their constituents, not just the party faithful. The system has been called “instant-runoff” voting because of the ability to consider voters’ second, third and fourth choices instantaneously. Now it’s increasingly looking like it might have the secondary benefit of removing the need for the state to pay for an additional statewide election every year.





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Alaska

Alaska and NW Canada Cold Snap Review

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Alaska and NW Canada Cold Snap Review


Most of December and the first two weeks of January were very cold in most of Alaska and northwest Canada. I posted about the cold in the first half of December here, the cold snap through Christmas here, December overall for Alaska here and Arctic context for the cold snap in the December climate review here.

This post serves as an event recap, though because of the breath and duration of event this review is necessarily selective. Also I have only limited tools to assess the historical context of this event in northwest Canada, so I’ve surely missed some important highlights. Because this event was international scope, I provide temperature information in both degrees F and degrees C. This makes the post longer, but I hope it’s relevant whatever your preferred temperature scale.

The 2025-26 cold snap was distinguished primarily by the long duration of the very cold weather rather than daily extremes. Based on ERA5 Land reanalysis, for Alaska overall, every day but two between December 4 and January 15 was colder than the 1991-2020 baseline average (Fig. 1 top), making this the most significant prolonged cold snap since 2012 (which was colder). For the Yukon Territory, every day between December 5 and January 9 was colder than average (Fig. 1 bottom).

Fig. 1 Daily average temperature difference from the 1991-2020 baseline average December 4, 2025 to January 20, 2026 for Alaska (top) and the Yukon Territory (bottom). Data from ERA5 Land courtesy of ECMWF/Copernicus

The coldest period for northwest North America overall was December 5 to January 15 (Fig. 2). The departures are quite markable given this is a seven week period.

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Fig. 2 Average temperature departure from 1991-2020 baseline average for the seven weeks December 5, 2025 to January 15, 2026. For Alaska and the Yukon Territory overall, this was the coldest 42 day period during this cold snap. Data from ERA5 Land courtesy of ECMWF/Copernicus.

For the Yukon Territory overall the coldest day was December 22, with temperatures south of 65°N widely 20°C or more below normal (Fig. 3). The very low temperatures extended into the eastern Interior, but Alaska west of about 160°W was notably warmer than normal.

Fig. 3 December 22, 2025 average temperature difference from the smoothed 1991-2020 average, degrees F (top) and degrees C (bottom). Data from ERA5 Land courtesy of ECMWF/Copernicus.

The coldest day from the central Yukon Territory westward into eastern and central Interior Alaska was January 4th (Fig. 4). Temperatures in southern YT were not quite as low as around winter solstice. With above normal temperatures across the Alaska Peninsula this wasn’t quite coldest day for Alaska overall.

Fig. 4 January 4, 2026 average temperature difference from the smoothed 1991-2020 average, degrees F (top) and degrees C (bottom). Data from ERA5 Land courtesy of ECMWF/Copernicus.

The coldest day for Alaska overall was January 8, anchored by the deep cold over southwest mainland but temperatures widely 15°F (9°C) or more below normal over mainland Alaska (Fig. 5). At this point temperatures had moderated considerably in the Yukon Territory and Southeast Alaska.

Fig. 5 January 8, 2026 average temperature difference from the smoothed 1991-2020 average, degrees F (top) and degrees C (bottom). Data from ERA5 Land courtesy of ECMWF/Copernicus.

The lowest temperatures recorded during December and January (Fig. 6) were notable, though not to record levels across Interior Alaska and the Yukon Territory. Both Tok and Chicken, Alaska, with lows of -63F (-52.8C), recorded the lowest temperatures at their respective locations since January 2009. Fairbanks’ and Tanana’s lowest temperature was the same as the low in 2024, and Bettles had a lower temperature last winter. Carmacks, YT reported the lowest temperature since 1996 but Whitehorse, Dawson, Beaver Creek and Pelly Crossing all had the lowest temperature only since 2022.

Fig. 6 plot of site specific lowest temperature reported in December 2025 and January 2026 in degrees F (top) and degrees C (bottom).

Beyond the Yukon and Interior Alaska there were a few daily records and other short term extremes during this cold snap.

Juneau airport low temperature of -10F (-23.3C) on December 22 and 23 were daily record lows and also the lowest temperature there since 1995.

In Southcentral Alaska there were a scattering of daily record lows the first and second weeks of January. Talkeetna set a daily record of -38F (-38.9C) on January 8. This is the first daily record low to be set in January since 1975. Also notable was the exceptionally cold January 3rd at Portage Glacier Visitor Center southeast of Girdwood. Calm winds and clear skies allowed the temperature to stay low all day, with a high temperature of -22F (-30.0C) and a low of -30F (-34.9C) the coldest day at this location since the observation site was established in 1998, though January 1989 probably had at least one day as cold or colder. Kenai’s low temperature of -36F (-37.8C) on January 8 wasn’t a daily record but it was the lowest temperature there since 1999.

In Southwest Alaska, King Salmon set daily record lows on two days and Bethel on one day.

The duration of cold snap is illustrated in these site-specific highlights:

  • Fairbanks Airport:

    • 21 days with lows of -40F/C or lower, all between December 14 and January 13, the most since the winter of 1970-71

    • 57 hours with dense ice fog (visibility one-quarter mile or lower), the most since the winter of 2008-09

    • 30-day average temperature -31.0F (-35.0C) December 15 to January 13, the lowest since 1970-71

  • Tok: 22 days with lows of -50F (-45.6C) or lower, all between December 8 and January 6

  • Chicken: 29 days with lows of -40F/C or lower, all between December 6 and January 10

Notable “consecutive days” streaks include:

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  • Fairbanks Airport:

    • 32 straight days high temperature 0F (-17.8C) or lower (December 14 to January 14), second longest on record

    • 43 straight days with daily low temperature -10F (-23.3C) or lower (December 4 to January 15), second longest on record

  • Tanana:

  • Eagle (cooperative station):

    • 42 straight days with daily high temperature 0F (-17.8C) or lower, (December 5 to January 15), longest on record

  • Northway:

  • Anchorage:

  • Dawson, YT: 19 straight days with lows -40F/C or lower, longest since 1996

The daily temperature ranges are shown at Fairbanks and Tok (Fig. 7). Fairbanks, the westernmost location shown, had two notable moderating events in December, both associated with pulses of warmer air aloft moving from the Bering Sea into the central Interior and both produced significant snowfall. The first of these made as far east as Tok. Also notable at all these valley locations are a number of very cold days with only a few degrees spread between the high and low temperature. These days were clear (excepting local ice fog) and calm and vividly illustrates that although the sun scraps above the horizon for a few hours, in December and early January this provides no significant solar heating poleward of 60°N.

Fig. 7 daily low to high temperature (blue bars) and 1991-2020 normal (gray band) between December 4, 2025 to January 15, 2026 at Fairbanks (top) and Tok (bottom). Data courtesy NOAA.NWS and NCEI.

The cold was particularly unrelenting at Dawson, YT in December (Fig. 8, top), although the coldest day occurred on January 4. At Whitehorse (Fig. 8, bottom), there we two distinct episodes of deep cold, one in early December and another around winter solstice.

Fig. 8 daily low to high temperature (blue bars) and 1991-2020 normal (gray band) between December 4, 2025 to January 15, 2026 at Dawson (top) and Whitehorse (bottom). Data courtesy Environment and Climate Change Canada.

An historical perspective on this cold snap at Fairbanks is shown in the times series plotting the coldest 10-day periods each winter since the early 1900s (Fig. 9). By this measure, this cold snap was slightly colder than 2011-12 and not quite as cold as 1988-89. However, about a dozen winters prior to 1980 had a 10-day period colder than this event.

Fig. 9 Fairbanks lowest 10-day average temperature each winter 1905-06 to 2025-26. A few winters are missing prior to 1916 due to excessive missing data. Data courtesy NOAA/NCEI and NWS.

The mid-atmospheric flow pattern and its slow evolution in December and January explains a lot of what happened on the ground. During the second half of December (Fig. 10, left) extremely strong high pressure aloft over the Bering Sea supported high pressure at the surface over eastern Interior Alaska and the Yukon. Because of the lack of solar heating, clear skies allowed continuous escape of heat from the top of the snowpack to outer space, with the cold air pooling in valleys. In early January (Fig 10, right) the pattern changed, with a general westward shift of the high and low pressure centers aloft compared to December. For example, the the Being high pressure shifted northwest to be near the Sea Of Okhotsk, while the low pressure over central Arctic Canada in December shifted west to be over the Beaufort Sea in early January. This westward “retrogression”, so-called because it’s in contrast to the more usual west-to-east progression of mid-latitude weather features near ground, is a common feature of the mid-atmosphere flow pattern during the cold season.

Fig. 10 Average 500 hPa heights and departures from 1991-2020 baseline for the second half of December (left) and the first half January (right). Data from the NCAR/NCEP R1 reanalysis data courtesy NOAA/ESRL.



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Photos: Alaska Ski For Women celebrates 30 years of costumes, camaraderie and community

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Photos: Alaska Ski For Women celebrates 30 years of costumes, camaraderie and community


Hundreds of women and girls skied at Kincaid Park on Sunday for the annual fundraiser.

“Greenland Defense Front” placed third in the team costume contest during the Alaska Ski For Women on Sunday, Feb. 1, 2026. (Bill Roth / ADN)

Hundreds of women took to the freshly groomed trails at Anchorage’s Kincaid Park in the sunshine Sunday to celebrate 30 years of costumes, camaraderie and community.

The Alaska Ski for Women is a fundraising event that supports the Nordic Skiing Association of Anchorage and Alaska nonprofits working to end the cycle of domestic violence in our community.

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Women and girls gather in the Kincaid Park stadium for the costume parade on Sunday. (Bill Roth / ADN)
Start of the freestyle (skate) race during the 30th Alaska Ski For Women at Kincaid Park on Sunday. (Bill Roth / ADN)
Leah Besh won the freestyle race during the 30th Alaska Ski For Women at Kincaid Park on Sunday. Besh also placed second in the classic race. (Bill Roth / ADN)
The classic race begins during the Alaska Ski For Women at Kincaid Park on Sunday. (Bill Roth / ADN)
From left, Leah Besh, Olympian Sue Forbes, and Grace Post celebrate on the podium after the classic race during the Alaska Ski For Women at Kincaid Park on Sunday. (Bill Roth / ADN)
The Alaska Ski For Women celebrated 30 years of costumes, camaraderie and community on Sunday. (Bill Roth / ADN)
“Happy 30th” won the team costume contest during the Alaska Ski For Women at Kincaid Park on Sunday. (Bill Roth / ADN)
“Viking skiing Mothers and Daughters of Norway” gather before the costume parade during the Alaska Ski For Women at Kincaid Park on Sunday. (Bill Roth / ADN)
The “Shrimp on the Barbie” team skis during the costume parade at Alaska Ski For Women on Sunday. (Bill Roth / ADN)
The Alaska Ski For Women event celebrated 30 years on Sunday. (Bill Roth / ADN)
The Alaska Ski For Women celebrated 30 years of costumes, camaraderie, and community on Sunday. (Bill Roth / ADN)
Costumed skiers participate in the Alaska Ski For Women on Sunday. (Bill Roth / ADN)
The party wave skis through the stadium at Kincaid Park during the Alaska Ski For Women on Sunday. (Bill Roth / ADN)
The party wave hits the trails at Kincaid Park during the Alaska Ski For Women on Sunday. (Bill Roth / ADN)

Bill Roth

Bill Roth is a staff photojournalist at the Anchorage Daily News.

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Twenty years of Arctic report cards

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Twenty years of Arctic report cards


Twenty years have passed since scientists released the first version of the Arctic Report Card, now a staple at the Fall Meeting of the American Geophysical Union.

Way back in 2006, at the Moscone Center in San Francisco, National Oceanic and Atmospheric Administration press people handed a paper version to reporters. Now it is a digital affair, more than 100 pages.

Since the late 1970s, the University of Alaska Fairbanks Geophysical Institute has provided this column free in cooperation with the UAF research community. Ned Rozell ned.rozell@alaska.edu is a science writer for the Geophysical Institute.



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