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Warm favourite

26.10.2001


The smart money is on global warming.


The Nenana Ice Classic tripod sinks into the frozen Tenana River.
© Julie Coghill.


Community ice breaker: a lot less exciting than it used to be.
© Julie Coghill.



An Alaskan sweepstake has become a record of global warming. The competition to predict when ice will melt reveals that, on average, the thaw comes more than five days earlier now than it did 84 years ago1.

In the winter of 1917, railway engineers working in Nenana, Alaska whiled away the long winter nights by erecting a wooden tripod on the frozen Tenana River and placing bets on the exact moment in spring when it would fall through the ice.


The Nenana Ice Classic, as it is now known, has taken place every year since. It attracts entrants from around the world and the original $800 jackpot (about $11,000 in current terms) has grown to around $300,000. The eight entrants who correctly predicted that this year the tripod would fall at 1 pm on 8 May pocketed $38,500 each.

Raphael Sagarin, of Stanford University in California, happened upon this unusual climate record while leafing through his Lonely Planet guidebook. "I was doing research on tide pools in southeast Alaska when I read about this competition," he says. "I thought it might be a good record of climate change."

The Classic stands up to scientific scrutiny because it measures the same thing every year with extreme precision. The contest ends when the tripod is swept downriver and trips a wire that stops a clock. The amount of money riding on the outcome also ensures accuracy.

The record includes a cooler spell in the middle of the century, and reflects rapid recent warming. Since 1975, the date at which the clock stops has advanced by about nine days.

"Ice melt is very strongly related to climate," says Tim Sparks of the Centre for Ecology and Hydrology in Monks Wood, Cambridgeshire, UK. Measuring melting in this way is "perfectly legitimate", adds Sparks, a champion of the contribution that amateur naturalists can make to climate monitoring.

"It’s just a piece of the whole puzzle," says Sagarin. Combined with information from other biological or physical processes, such as leaf budburst and lake-ice melting, "it shows that the timing of the natural world is moving earlier".

Thaw point

The trend is not predictable enough to aid punters - this year the tripod lasted well beyond the 1917 date of 30 April, for example. Sagarin himself has not entered: "I wondered if I’d have an unfair advantage, but there’s no science to guessing in an individual year."

Two forces can bring about the tripod’s downfall. The ice beneath it can melt or floes swept down the river can break it up. From talking to local witnesses, Sagarin concludes that the former has become more common. Now the ice "just sort of rots away" beneath the tripod, he says. One person told him that the ice contest is "a lot less exciting than it used to be".

References
  1. Sagarin, R. & Micheli, F. Climate change in nontraditional datasets. Science, 294, 811 (2001).

JOHN WHITFIELD | Nature News Service
Further information:
http://www.nature.com/nsu/011101/011101-2.html
http://www.nature.com/nsu/

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