Arctic Sea Ice Extent
1. Sea ice extent is a measure of the surface area of the ocean covered by sea ice. Increases in air and ocean temperatures decrease sea ice extent; in turn, the resulting darker ocean surface absorbs more solar radiation and increases Arctic warming.
2. The minimum sea ice extent in the Arctic, measured in September of each year, has decreased by about 36% since 1979. The September 2016 sea ice extent was more than 700,000 square miles less than the historical 1981–2010 average for that month—a difference more than two and a half times the size of Texas.
Sea ice extent is estimated using daily satellite images to calculate the total ocean area that has an ice concentration of 15% or more. Trends in sea ice extent shown here are calculated from average values measured during the month of September, which is typically when sea ice extent reaches its annual minimum thickness and extent. Minimum sea ice extent in the Arctic has decreased by about 36% since 1979 (the first full year of satellite data). At this rate, some projections suggest that the Arctic will be virtually ice-free during summers by the middle of this century.
The melting of sea ice reduces the area of white surface that reflects the sun’s radiation, simultaneously increasing the area of dark ocean surface that absorbs it. This albedo effect results in a cycle of further sea ice melt and more warming of the ocean. Before melting begins, snow-covered sea ice absorbs only about 20% of the solar radiation that reaches it, whereas the ice-free ocean surface absorbs over 90%. A warmer ocean may melt ice from below, or may release heat back into the atmosphere before the ocean refreezes in the winter—leading over time to less sea ice and a warmer climate.
The loss of sea ice also increases the