The amount of sea ice in the Arctic has fallen to the lowest level on record, a confirmation of the drastic warming in the region and a likely harbinger of larger changes to come.
Satellites tracking the extent of the sea ice found over the weekend that it covered about 1.58 million square miles, or less than 30 per cent of the Arctic Ocean's surface, scientists said.
That is only slightly below the previous record low, set in 2007, but with weeks still to go in the summer melting season, it is clear that the record will be beaten by a wide margin.
The National Snow and Ice Data Centre, a government-sponsored research agency in Boulder, Colorado, announced the findings last night in collaboration with Nasa.
The amount of sea ice in summer has declined more than 40 per cent since satellite tracking began in the late 1970s, a trend that most scientists believe is primarily a consequence of human activity.
"It's hard even for people like me to believe, to see that climate change is actually doing what our worst fears dictated," said Jennifer A Francis, a Rutgers University scientist who studies the effect of sea ice on weather patterns.
"It's starting to give me chills, to tell you the truth."
Scientific forecasts based on computer modelling have long suggested that a time will come when the Arctic will be completely free of ice in the summer, perhaps by the middle of the century.
This year's prodigious melting is lending credibility to more pessimistic analyses that it may come much sooner, perhaps by the end of the decade.
"It's an example of how uncertainty is not our friend when it comes to climate-change risk," said Michael E Mann, a climate scientist at Pennsylvania State University.
"In this case, the models were almost certainly too conservative in the changes they were projecting, probably because of important missing physics."
Experts say that a large storm in the Arctic this summer may have contributed to setting the record. But it would not have happened, they say, if the ice had not been steadily contracting for the past several decades.
The pace of that decline seems to be accelerating.
But scientists are somewhat cautious in their predictions, given that sea ice is prone to natural variability.
They have only a 33-year record of careful satellite observations, and before that, only sketchy data from maps and other historical sources.
By itself, the melting of sea ice does not raise global sea levels, because the floating ice is already displacing its weight in seawater. But the sharp warming that is causing the sea ice to melt also threatens land ice, notably the Greenland ice sheet, which is melting at what appears to be an accelerating pace, and melting land ice does raise sea levels.
Already, the reduction in sea ice is altering weather patterns in the Arctic region, and perhaps beyond.
It is stressing the ecology of the region and causing rapid erosion of shorelines that are now exposed to more vigorous waves.
The melting does, however, offer some potential benefits, including new shipping routes and easier access to oil and other mineral deposits.
A rush is under way to stake claims and begin mineral exploration in the Arctic.
The average temperature of the region is rising more than twice as fast as that of the earth as a whole, confirming a prediction first made in 1896: that increasing levels of carbon dioxide from the burning of fossil fuels would have an especially large impact in the Arctic.
One reason is that the white surface of the ice reflects a great deal of the sunlight that strikes it back into space, but the darker water and land exposed when the ice melts absorbs more heat from the sun, which in turns leads to additional melting, more sunlight absorption and so on - a feedback loop that scientists call Arctic amplification.
Ms Francis is one of a small group of climate scientists who argue that the decline of sea ice is already having consequences for weather in the Northern Hemisphere's middle latitudes, including the United States.
She has published research suggesting that air circulation patterns are being altered in a way that favours more extremes, like heat waves and droughts.
Such ideas are not considered proven, but they are getting more attention as the weather careens from one extreme to another.
Every year, the surface of the Arctic Ocean freezes during the long, dark winter, with the extent of sea ice usually peaking in March.
Until recent decades, the ice was so thick by that time of year that a high proportion of it would survive the summer.
But scientists say the warming trend has now reduced the ice to just a shell in many places.
That means it can melt easily in the round-the-clock sunshine that strikes the highest latitudes in summer.
"Parts of the Arctic have become like a giant Slushee this time of year," Walt Meier, a top scientist at the snow and ice centre said.
New York Times