TheGulf of Riga,[a] also known as theBay of Riga or theGulf of Livonia, is a bay of theBaltic Sea betweenLatvia andEstonia.
The island ofSaaremaa (Estonia) partially separates it from the rest of the Baltic Sea. The main connection between the gulf and the Baltic Sea is theIrbe Strait.
Major islands in the gulf includeSaaremaa,Kihnu, andRuhnu, which are all inEstonian territory. Kihnu covers an area of 16.4 square kilometres (6.3 sq mi).[4] Saaremaa island is responsible for the brackish water of the Gulf of Riga, as it is partially "shielded" from the Baltic Sea. The Baltic itself is already less salty than the global oceanic average, but this effect has a north–south and east–west gradient.[5][6]
The freshwater runoff entering the Baltic sea accounts for two percent of its volume.[4] A narrow connection to the North Sea means that water stays in the Baltic for an average of 30 years. These two characteristics work to make the Baltic Sea one of the largestbrackish bodies of water in the world. The Gulf of Riga has an average salt concentration for the Baltic Sea, which is around six to ten parts per thousand. Freshwater has a concentration of 0.5 parts per thousand, and seawater is about 30 parts per thousand.[4]
In winter, most or all of the Bay occasionally freezes. This is due to low salinity and the calming effect of the partial closure of the entrance of the gulf. During the winter, many people walk over the bay. The thickest recorded ice was 90 centimetres (2 ft 11 in) thick in the winter of 1941–42.[7] Ice hole fishing has been a traditional source of winter food, and remains a common activity. The ice usually melts between March and April. In late March 2013, when the ice started to melt, 200 people had to be rescued from ice floes.[8]
^abcC.Michael Hogan. 2011.Gulf of Riga. Encyclopedia of Earth. Eds. P.Saundry & C.J.Cleveland. National Council for Science and the Environment. Washington DC.
