Somali Current Somali Current The Somali Current is an ocean boundary current that runs along the coast of Somalia and Oman in the Western Indian Ocean and is analogous to the Gulf Stream in the Atlantic Ocean. This current is heavily influenced by the monsoons and is the only major upwelling system that occurs on a western boundary of an ocean. The water that is upwelled by the current merges with another upwelling system, creating one of the most productive ecosystems in the ocean. The Somali current is characterized by seasonal changes influenced by the Southwest monsoon and the Northeast Monsoon. During
Western Europe Atlantic Current. Western European languages mostly fall within two Indo-European language families: the Romance languages, descended from the Latin of the Roman Empire; and the Germanic languages, whose ancestor language (Proto-Germanic) came from southern Scandinavia. Romance languages are spoken primarily in the southern and central part of Western Europe, Germanic languages in the northern part (the British Isles and the Low Countries), as well as a large part of Northern and Central Europe. Other Indo-European languages include the Celtic group (that is, Irish, Scottish Gaelic, Manx, Welsh, Cornish, and Breton). Basque is the only currently living Western European language isolate.