Prince Christian Sound


The Prince Christian Sound is a waterway in Southern Greenland.
It separates the mainland from Sammisoq and other islands of the Cape Farewell Archipelago near the southernmost tip of Greenland. The name was given in honour of the prince, later king Christian VIII of Denmark.

Geography

The Prince Christian Sound connects the Labrador Sea with the Irminger Sea. It is around 100 km long and it is narrow, sometimes only wide. There is only one settlement along this sound, Aappilattoq.
The long fjord system is mostly surrounded by steep mountains in general reaching over, one of them high Many glaciers go straight into its waters where they calve icebergs. There are often strong tidal currents limiting the formation of ice. It has many offshoots, such as Kangerluk to the north midway through the fjord, Ikeq Fjord in the south, and in the west Ilua Fjord, Ikerasaq Fjord, Utoqqarmiut Fjord and the Torsukattak Fjord.

Weather station

At the entrance to the East to the Strait there is a weather station founded by the US during World War II under the name Bluie East One. The task of the weather station was to ensure that the shipping industry had reliable data on the weather at Cape Farewell, Greenland. On January 7, 1959, when the ship MS Hans Hedtoft hit an iceberg at Cape Farvel, the radio telegraphist at the weather station at Prince Christian Sound was the first to catch the ship's distress signal.
The weather station is today run by the International Civil Aviation Organization ICAO together with Tele Greenland. A long wooden stairway leads from the harbour up to the station with community building, power plant, residential barracks and radio aerial plants.

Tourism

The scenery of Prince Christian Sound attracts summer cruise ships to the area, with some vessels as large as the 86,700 ton Eurodam. Ships must go slowly due to the icebergs.

Climate

Prince Christian Sound has a maritime polar climate making borderline with subpolar oceanic climate due low annual temperature swings for its latitude and relatively high temperature in center months. Summer temperatures are way below the tree line requirements, whereas the long winters are comparatively mild for its high latitude. The nearby ice sheet produces cold air which keeps summer temperatures down.