Warm weather caused substantial melting in June and July 2023, especially on the southern portion of the island.
More than halfway through the 2023 melting season, G a significant transformation of Greenland’s snow cover has been observed. There has been above-average melting throughout most of the season. Notably, on several days in June and July, melt was detected across up to 50 percent—equivalent to 800,000 square kilometers (302,000 square miles)—of the Greenland Ice Sheet’s surface. This is according to data comes from the National Snow and Ice Data Center.
The Impact on Frederikshåb Glacier
Summer melting was ramping up on June 14, 2023, when Landsat 8’s Operational Land Imager (OLI) acquired this image (top) of Frederikshåb Glacier. This lobe-shaped piedmont glacier, located in southwest Greenland, flows downward from the Greenland Ice Sheet, winds past a series of valleys and nunataks, then flattens out on smoother terrain along the coast.
The other image (lower), acquired with the OLI-2 on Landsat 9, shows the same area on July 24, after more than a month of additional melting. There is a dramatic reduction in the extent of brighter (high albedo) surface snow that is easily noticed.
Increased Monitoring Capabilities With Landsat 9
Since September 2021, when Landsat 9 joined Landsat 8 in orbit over Earth, scientists have been getting more frequent detailed views of Earth. The Landsat 8 and Landsat 9 satellites together acquire about 1,500 scenes from across the planet every day. That comes in handy for observing the planet’s icy regions, where seasonal changes can be quick and dramatic.
Transition From “Clean” Snow to “Dirty” Ice
Another seasonal change visible in the image pair above is the transition from “clean” snow to “dirty” ice. One reason for the darker color is due to the presence of particles, such as black carbon or dust, that have accumulated on the ice. As the snow and ice melt, these impurities are left behind. Darkening of the ice surface lowers its albedo, which can hasten melting through the absorption of additional solar energy in the summer months.
Appearance of Melt Ponds
Another noticeable change is in the emergence of ponded water, or “melt ponds,” on the surface of the ice sheet. Deep blue in color, they form where snow has melted and pooled in low spots on the ice sheet’s undulating topography. They can be an important indicator of the strength of Greenland’s melting season, which generally runs from May to early September.
Only a few melt ponds are visible in the July 24 image (top-lower), possibly because meltwater had already run off the ice sheet or been channeled down through the ice. However, abundant melt ponds were visible about 100 kilometers (60 miles) north of Frederikshåb on July 8, when the OLI-2 on Landsat 9 acquired the image above.
Impact of Seasonal Weather Changes
These transformations are consequences of the increase in summer warmth that set in across the region in late June. At that time, warm southwesterly winds and clear skies significantly intensified the amount of melting on the ice sheet, especially towards the island’s south.
Comparison With Previous Melting Seasons
So far in Greenland’s 2023 melting season, spikes in daily melt area have stayed below those of 2012, a year with exceptionally widespread melting. Still, as of mid-July, daily melt extents have been consistently higher than the 1981-2010 average, and 2023 is on par with several other high melt years in recent decades.
“The drama of unprecedented melt in 2012 may not be exceeded this year,” said Christopher Shuman, a University of Maryland, Baltimore County, glaciologist based at NASA’s Goddard Space Flight Center. “But so far, 2023 looks to be a big, broad melt year.”
NASA Earth Observatory images by Wanmei Liang, using Landsat data from the U.S. Geological Survey.