The Prince Gustav Channel (63°50′S 58°15′W) was named in 1903 after Crown Prince Gustav of Sweden (later King Gustav V) by Otto Nordenskiöld of the Swedish Antarctic Expedition. Gustaf V (Oscar Gustaf Adolf) (June 16, 1858 – October 29, 1950) was King of Sweden from 1907 until his death. ... Dr Nils Otto Gustaf Nordenskiöld (also spelled Nordenskjöld) (December 6, 1869-1928) was a Swedish geologist, geographer, and polar explorer. ... The expedition (1901-1904) was led by Otto Nordenskjöld and Carl A. Larsen (the captain of the ship Antarctic). ...

The channel is bounded on the west by the Antarctic Peninsula and on the east by James Ross Island. It is about 80 miles long and ranges from 4 to 15 miles wide. Map of Ross Island Ross Island is a volcanic island in the Ross Sea by Antarctica, on the coast of Victoria Land. ...

On February 27th, 1995, the British Antarctic Survey (BAS) reported that an ice shelf formerly blocking the channel had disintegrated. This ice shelf had spanned approximately 270 square miles prior to its disintegration. BAS headquarters The British Antarctic Survey (BAS), formerly the Falkland Islands Dependencies Survey (FIDS), is an institute of the Natural Environment Research Council, and has, for the last fifty years, undertaken the majority of Britains scientific research on and around the Antarctic continent. ...

In the area previously covered by the shelf, the channel's water depth is between 600 and 800 meters. Between February and March 2000 scientists collected sediment cores 5 to 6 m in length from the ocean floor. Carbon dating of organic material found in the sediment layers suggested that for a period between 2,000 to 5,000 years ago, much of the channel was seasonally open water. While icebergs were able to navigate the channel, ice rafted debris was deposited within the sediment.

It appears that before and after this period, the channel remained closed. The period when the channel was open coincides with a period of local warming supported by data gathered from land-based studies of lake sediments and ancient, abandoned penguin rookeries. With the return of colder conditions about 1900 years ago, the Prince Gustav ice shelf reformed until its recent retreat.

Ice shelves are sensitive indicators of regional climatic change, therefore recent warming in the vicinity of the Prince Gustav Channel is exceptional for at least the past 1900 years.