White Sea
Southern inlet of the Barents Sea, key to Russian maritime trade.
The White Sea cuts into Russia’s northwest coast as a southern arm of the Barents Sea. It is bounded by Karelia on the west, the Kola Peninsula to the north, and the Kanin Peninsula to the northeast. Entirely within Russian territory, it is classified as internal waters and split administratively among Arkhangelsk and Murmansk oblasts and the Republic of Karelia. Arkhangelsk, a key port on this sea, served for centuries as Russia’s primary hub for overseas trade, run by the Pomors from Kholmogory. Later, it became a major Soviet naval and submarine base. A canal, the White Sea–Baltic, links this sea to the Baltic. Along with the Black, Red, and Yellow seas, it is one of four bodies of water named after a common color term.
The International Hydrographic Organization sets the White Sea’s northern boundary as a line from Svyatoy Nos on the Murmansk Coast to Cape Kanin. The sea has four main bays, all connected to the Barents Sea through a funnel-shaped opening and a narrow strait called Gorlo—Russian for “throat.” Kandalaksha Gulf, in the west, is the deepest part at 340 meters. To the south, Onega Bay receives the Onega River. Southeast lies Dvina Bay, where the Northern Dvina flows into Arkhangelsk. On the east side of the gorlo, opposite the Kola Peninsula, Mezen Bay takes in the Mezen and Kuloy rivers. Other major rivers include the Vyg, Niva, Umba, Varzuga, and Ponoy.
The central seabed and Dvina Bay are covered in silt and sand, while the northern part, Kandalaksha Gulf, and Onega Bay have a mix of sand and stones. Ice age deposits often appear near the shores. Northwestern coasts are tall and rocky, but the southeastern side slopes more gently. Many small islands dot the sea; the largest group is the Solovetsky Islands, near the entrance to Onega Bay. Kiy Island in Onega Bay is notable for a historic monastery, and Velikiy Island, close to shore, is the biggest in Kandalaksha Gulf.
The White Sea sits in a depression on the Baltic Shield continental shelf. Its bottom is uneven, with the Kandalaksha Hollow in the northwest and the Solovetsky Islands in the south. Onega Bay has many small underwater rises. The sea’s opening and the gorlo are shallow, around 50 meters or less. An underwater ridge in the northern gorlo limits depths to 40 meters, restricting water exchange with the Barents Sea. Tides, which occur twice daily, help this exchange; their amplitude ranges from 1 meter in the south to 10 meters in Mezen Bay. Open-sea currents are weak, under 1 km/h, but strengthen in the bays. Tidal waves are faster, reaching 9 km/h in Mezen Bay, 3.6 km/h in Onega Bay, and 1.3 km/h in Kandalaksha Gulf.
Rivers deliver about 215 km³ of fresh water annually, mostly to Onega, Mezen, and Dvina bays. The Northern Dvina alone can contribute up to 171 km³ in some years, with the Mezen, Onega, Kem, and Vyg adding 38.5, 27.0, 12.5, and 11.5 km³, respectively. About 40% of this volume arrives during May snowmelt, with minimal inflow in February and March. This seasonal flow raises and lowers sea level, promoting exchange with the Barents Sea. Each year, roughly 2,000 km³ flows into the White Sea and 2,200 km³ flows out. Spring freshwater inflow lowers surface salinity in the top 5–10 meters to 23‰ in the east, 26–27‰ in the west, and 10–12‰ in Dvina Bay, while also increasing silicon and silicate content—a characteristic feature.
Storms peak in October and November. Shallow depths keep average wave height at 1 meter, occasionally reaching 3–5 meters. The sea is calm in July and August. The climate is polar to subarctic, with frequent fog and clouds. Winter winds are mostly southwestern at 4–8 m/s, bringing cold air from the south and temperatures around −15°C in February over most of the sea. The north is warmer, about −9°C, sometimes −6°C, due to Atlantic air masses. Arctic anticyclones shift winds to the northeast, bringing colder weather near −25°C. Summers are cold, cloudy, and humid, with northeastern winds and frequent rain. Average July temperatures are 8–10°C. Occasional southeastern winds from Europe can raise temperatures to 17–19°C, sometimes 30°C. Annual precipitation ranges from 282 mm in the north to 529 mm in the south.
From October–November to April–May, the sea freezes. Average January water temperatures are −1.9°C in the north, −1.3 to −1.7°C in the center, and −0.5 to −0.7°C in the bays. These differences reflect salinity variations: 24–26‰ in the center, 30.5‰ in the gorlo, and 34.0–34.5‰ toward the Barents Sea. The freezing period varies yearly, and the ice is not stationary.
- Type
- Sea (inlet of Barents Sea)
- Location
- Northwest coast of Russia
- Maximum depth
- 340 metres (Kandalaksha Gulf)
- Major port
- Arkhangelsk
- Area classification
- Internal waters of Russia
- Administrative divisions
- Arkhangelsk and Murmansk oblasts, Republic of Karelia
Lore & Background
The White Sea is a water-filled depression in the block of a continental shelf known as the Baltic Shield. Its bottom is very uneven and contains the Kandalaksha Hollow in the northwest and the Solovetsky Islands in the south. There are four main bays or gulfs on the White Sea: Kandalaksha Gulf, Onega Bay, Dvina Bay, and Mezen Bay. These bays connect with the funnel-shaped opening to the Barents Sea via a narrow strait called 'Gorlo'. Kandalaksha Gulf is the deepest part of the sea, reaching 340 metres. The seabed of the central part and Dvina Bay is covered in silt and sand, whereas the bottom of the northern part, the Kandalaksha Gulf and Onega Bay is a mixture of sand and stones. Ice age deposits often emerge near the sea shores. Northwestern coasts are tall and rocky but the slope is much weaker at the southeastern side. The White Sea contains a large number of islands, but most of them are small. The main island group is the Solovetsky Islands, located almost in the middle of the sea, near the entrance to Onega Bay. Kiy Island in Onega Bay is significant due to a historic monastery. Velikiy Island, located close to the shore, is the largest island in the Kandalaksha Gulf.
Reader's Guide
Residents of Novgorod knew of the White Sea from at least the 11th century and rapidly explored its commercial significance for navigation and its coastal forests rich in fur animals. One of the earliest settlements near the sea shores grew up in the late 14th century at Kholmogory, on the Northern Dvina. From there, in 1492, a merchant fleet laden with grain and carrying ambassadors of Ivan III of Russia sailed to Denmark, marking the establishment of the first international seaport in Russia. The first foreign ship to arrive in Kholmogory was the English Edward Bonaventure commanded by Richard Chancellor in 1553. Together with two other ships under the command of Hugh Willoughby, his crew had sought a northern route to the Indies, especially India and China. The expedition, sponsored by King Edward VI of England and a group of about 240 English merchants, had London's authorisation to establish trade connections. The ships of Willoughby were separated and the other two were lost at sea, but Edward Bonaventure managed to pass the White Sea and reach Kholmogory, from where Chancellor was escorted to Moscow to meet the Russian Tsar, Ivan IV. Returning from Russia in 1554, Chancellor brought back a detailed description of Moscow and the Russian north, which were largely unknown to Europe, as well as a letter from the Tsar expressing desire to establish trade relations with England. In 1555 Queen Mary issued a charter authorising the Muscovy Company to trade with Russia via the White Sea route. Dutch ships soon followed the English, and the port of Kholmogory became busy with shipments of fur and fish. Local and foreign shops and factories were established in the city at that time. The port was reinforced with a fortress which sustained a siege by the Polish-Lithuanian army in 1613. Increasing traffic overloaded the port, which relied on shallow river-waters and had limited ship-capacity. However, instead of expanding the old port, Ivan IV established a new one down-river in 1584, called New Kholmogory, which from 1596 began to become known as Arkhangelsk. Between the 15th and early 18th centuries, the White Sea served as the major trade route in and out of Russia. This role decreased later after the foundation of Saint Petersburg (1703), which opened a more direct ice-free connection between Russia and the bulk of Western Europe via the Baltic Sea. From the 1920s, most northern Russian sea shipments diverted from the White Sea to the new port of Murmansk (officially founded in 1916), where the waters did not freeze in winter.
Did You Know?
- The White Sea is one of the four seas named after common colour terms, alongside the Black, Red and Yellow seas.
- The narrow strait connecting the White Sea to the Barents Sea is called 'Gorlo', which means 'throat' in Russian.
- The first foreign ship to reach the White Sea was the English Edward Bonaventure, commanded by Richard Chancellor in 1553.
- The White Sea freezes from October–November to April–May, with ice thickness usually about 40 cm but reaching 150 cm in cold winters.
- The White Sea–Baltic Canal connects the White Sea with the Baltic Sea.
Frequently Asked Questions
What is the White Sea?
The White Sea is a partially enclosed body of water that acts as a southern extension of the Barents Sea. It sits tucked along Russia's northwestern coastline and is classified as internal Russian waters rather than open ocean.
Where exactly is the White Sea situated?
It lies on the northwest coast of Russia, bordered by the Karelian region to the west, the Kola Peninsula to the north, and the Kanin Peninsula to the northeast. The entire basin falls under Russian sovereignty.
How deep does the White Sea get?
Its deepest point reaches approximately 340 metres, found within the Kandalaksha Gulf. This makes it relatively shallow compared to many other seas.
Why was the White Sea historically significant for trade?
For centuries it served as Russia's primary gateway for international maritime commerce, with the Pomor communities operating out of Kholmogory as key trading hubs. The port city of Arkhangelsk remains its principal modern seaport.
Which regions does the White Sea belong to administratively?
The sea is split across three Russian administrative units: the Arkhangelsk Oblast, the Murmansk Oblast, and the Republic of Karelia. Despite this division, it remains a single internal water body under one national jurisdiction.
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