For most of the year, the Barnes Ice Cap\u00a0in the Canadian Arctic lies quiet under a blanket of snow. By summer, that snow melts back, and the ice cap transforms in texture, its bare ice dotted with turquoise ponds and its surface threaded with meltwater channels. In summer 2026, this seasonal awakening arrived fast and early.<\/p>\n
Located in the center of Baffin Island, the ice cap is a remnant of the Laurentide Ice Sheet, which once covered much of northern North America.\u00a0Today, the bowling-pin-shaped ice cap spans around 5,700 square kilometers (2,200 square miles), with ice up to about 730 meters (2,400 feet) thick. Like most of the glacial ice across the Canadian Arctic<\/a>, the Barnes Ice Cap is thinning and retreating<\/a>. \u00a0<\/p>\n The ice cap entered the 2026 melt season with an already-thin snowpack, and within a few weeks it had gone from snow-covered to mostly bare. By mid-July, its snow cover was effectively gone\u2014\u201cthe earliest it has been this bare,\u201d said glaciologist Mauri Pelto of Nichols College, who has monitored the ice cap<\/a> using images from Landsat satellites and, when possible, field observations.<\/p>\n<\/div>\n<\/div>\n<\/div>\n Once snow cover melts away and bare ice is exposed, melting speeds up in the Arctic summer sunshine. Bare ice is darker than snow and absorbs more solar energy, so as the reflective snow cover disappears, the ice cap warms and melts faster. At the same time, a network of meltwater channels, many of which persist from year to year, becomes increasingly visible.<\/p>\n The\u00a0OLI<\/a>\u00a0(Operational Land Imager) on\u00a0Landsat 9<\/a> acquired these images of the ice cap on July 12, 2026. Ponded blue meltwater dots the ice in places, and a vast network of meltwater channels spans the ice cap\u2019s surface from its middle to its edges. Faint, curving gray lines indicate the many millennia of snow and ice accumulation that built the ice cap.<\/p>\n Barnes Ice Cap has been snow-free before, including in 2019, 2020, and 2024, Pelto said, but this year it happened sooner. The early snow loss and return of meltwater channels in 2026 means that meltwater runoff is starting earlier too, with implications for the ice cap’s mass balance<\/a>. Water that might once have pooled and then percolated into any remaining snowpack and firn<\/a> and refrozen there\u2014adding mass back to the ice cap\u2014instead gets whisked away. That surface drainage becomes more efficient as the season progresses and channels widen and connect. <\/p>\n Research indicates<\/a> the\u00a0ice\u00a0cap\u00a0thinned roughly 1 meter (3 feet) per year from 2000 to 2020, and over the past 40 years its margin has retreated about 4 meters (13 feet) per year on average. However, retreat rates vary widely across the ice cap. An especially fast-retreating area on the ice cap\u2019s central-southern side pulled back by more than 400 meters (1,300 feet) total, or roughly 10 meters (33 feet) per year. This retreat is visible in the wide view above as a lighter brown band of freshly exposed earth and rock along that side of the ice cap.<\/p>\n NASA Earth Observatory images by Lauren Dauphin, using Landsat data from the\u00a0U.S. Geological Survey<\/a>. Story by Kathryn Hansen, with science review by Christopher Shuman, UMBC (retired).<\/em><\/p>\n Stay up-to-date with the latest content from NASA as we explore the universe and discover more about our home planet.<\/p>\n<\/p><\/div><\/div><\/div><\/div><\/div>\n![\"The](\"https:\/\/assets.science.nasa.gov\/dynamicimage\/assets\/science\/esd\/eo\/images\/iotd\/2026\/a-bare-summer-for-barnes-ice-cap\/barnesicecap_oli2_20260712_lrg.jpg?w=9891&h=6594&fit=clip&crop=faces%2Cfocalpoint\")
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