It’s official: When the sea ice that blankets the Arctic Ocean on Feb. 25, the maximum area was a record low.

Warm temperatures in parts of the polar regions kept sea ice levels depressed, and also contributed to the winter peak occurring much earlier than usual, the announced Thursday. The maximum normally isn’t reached until early March, but was recorded about a week early this year, the NSIDC said. That low occurred on the backdrop of overall dwindling sea ice levels, fueled by global warming.

The extent of Arctic sea ice is monitored by satellites throughout the year. Scientists keep a close eye on sea ice area because it is so crucial to the polar habitat and has considerable economic potential. Animals like polar bears and walruses depend on it to reach their food, and diminished ice makes the search for sustenance more difficult. Humans are interested in the opportunities afforded by ice melt in terms of new shipping lanes and oil drilling, much .

The record low winter sea ice extent of 2015 compared to the winter peaks of other recent years. (National Snow and Ice Data Center)

Changes in sea ice area have also been linked to over North America, Europe and Asia, though the connection is still tenuous.

The amount of the polar ocean covered by sea ice waxes and wanes with the seasons, reaching its lowest point at the end of summer and its peak at the end of winter. But this natural cycle has been affected by the rapid warming of the Arctic, which is happening at a much faster than the world as a whole.

As the Earth warms and ice melts, more areas of open ocean are created. The dark waters readily absorb the sun’s rays, whereas bright, white sea ice would reflect them. The heat absorbed by those waters melts more ice, creating a self-perpetuating cycle.

On average, Arctic sea ice extent has declined by 4.52 percent per decade, according to the NSIDC. The has seen an even steeper drop of 13.7 percent per decade.

The 2015 winter maximum was measured at 5.61 million square miles, which is 425,000 square miles lower than the 1981-2010 average and the lowest winter maximum in the satellite record, which extends back to the late 1970s. It was 50,200 square miles below the previous record low maximum, set in 2011.

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Extremely warm temperatures over the Pacific sector of the Arctic this winter — and linked to the heat that has baked the U.S. West — helped keep ice in those area much below normal.

In the first two weeks of March, temperatures were also unusually warm over parts of the Atlantic sector.

Those weather patterns contributed to the early peak, which while unusual, wasn’t unprecedented. In 1996, the peak occurred on Feb. 24.

Neither the winter maximum area nor its timing necessarily has an effect on the summer minimum. Research has shown little correlation between minimum and maximum areas, and 1996 actually was a banner year for summer extent.

“What is more important is how thick the ice is,” Julienne Stroeve, a NSIDC sea ice researcher said in an email.

Older, thicker ice is more likely to withstand the warmer temperatures of summer than younger, thinner ice. But the pressures of rapid warming have been, recent research has shown.

How the ice has fared in terms of thickness this winter is something the NSIDC is still analyzing and will release early next month.MORE FROM CLIMATE CENTRAL:

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Grinnell Glacier, Glacier National Park (1938 and 2009)

A side-by-side comparison of Grinnell Glacier in Montana's Glacier National Park. The black-and-white photo on the left dates from 1938, while the color photo on the right was taken in 2009. (T.J. Hileman and Lindsey Bengtson, USGS)