The National Snow and Ice Data Center reports that the Arctic melt season is now in high gear:
Through most of June, ice extent tracked close to two standard deviations below the long-term mean and just above the levels observed in 2007.

The graph above shows daily sea ice extent as of July 6, 2009. The solid blue line indicates 2009; the dashed green line shows 2007; and the solid gray line indicates average extent from 1979 to 2000. The gray area around the average line shows the two standard deviation range of the data.
NSIDC says that Arctic ice extent has been declining at a rate of 3.3% per decade:
Compared to previous Junes, ice extent in June 2009 was extremely close to the last two years, falling within 30,000 square kilometers (12,000 square miles) of the June extent in 2007 and 2008. The long-term trend indicates a decline of 3.3% per decade, an average of 40,100 square kilometers (15,500 square miles) of ice per year.

Monthly June ice extent for 1979 to 2009 shows a decline of 3.3% per decade.
In June, the Arctic saw warm temperatures over the Laptev Sea and the northern Beaufort Sea, while the Atlantic sector of the Arctic was slightly cooler than normal. The warm temperatures in the Laptev Sea corresponded to quickly declining ice concentrations in the area. NSIDC expects this region to become largely ice-free in the next few weeks.

The map of sea ice concentration from AMSR-E from July 5, 2009 shows low ice concentrations in the Laptev Sea, where atmospheric temperatures have been particularly warm in the month of June.
Arctic sea ice has thinned dramatically, some seven inches (17.8 centimeters) a year, or 2.2 feet (67 centimeters) between the winters of 2004 and 2008, according to a study by NASA and the University of Washington. The scientists also found that thicker, older ice, which has survived one or more summers, shrank by 42% – the equivalent of Alaska’s land area.
Thicker, older ice is less vulnerable than thinner ice to melting in the summer months. Less summer ice means more open water, which absorbs more heat, warming the ocean and further melting the ice.
Australian polar explorer Eric Philips reports:
Each year I guide ski expeditions across the pack ice to the North Geographic Pole and each year brings new surprises — severe storms rarely seen in these parts, vast tracts of first-year ice where there should be years of accumulation, pack ice drifting faster and farther than ever before.
The veneer of fractured ice over the Arctic Ocean is changing, disintegrating before my eyes.