where is the sea of japan

The surface layer tends to be more fresh in the sea parts which experience ice melting and rains. [12] The timing and extent of freezing vary from year to year, so ice may start forming in the bays as early as in October and its remains may be seen even in June. The tidal waves have a speed of 10–25 cm/s (3.9–9.8 in/s) in the open sea. Niigata is located two hours of Shinkansen from Tokyo and is the biggest port city on the Sea of Japan. The Northeastern limit of the Eastern China Sea [From Nomo Saki (32°35′ N) in Kyusyu to the South point of Hukae Sima (Goto Retto) and on through this island to Ose Saki (Cape Goto) and to Hunan Kan, the South point of Saisyu To (Quelpart), through this island to its Western extreme and thence along the parallel of 33°17′ North to the mainland] and the Western limit of the Inland Sea [defined circuitously as "The Southeastern limit of the Japan Sea"]. The Sea of Japan is a classic semienclosed sea, since its connections with adjacent bodies of water are greatly restricted by the narrow straits. Sea of Japan (East Sea) is a Real World random map introduced in Age of Empires II: The Conquerors. In summer the southerly tropical monsoon blows from the North Pacific onto the Asian mainland, causing dense fog when its warm and moist winds blow over the cold currents that prevail over the northern part of the sea at that season. [27] The south part of the Japanese archipelago remained as a relatively large landmass. Prominent capes include Lazareva, Peschanyi (sandy), Povorotny, Gromova, Pogibi, Tyk, and Korsakova in Russia; Crillon on Sakhalin; Sōya, Nosappu, Tappi, Nyuda, Rebun, Rishiri, Okushiri, Daso and Oki in Japan;[28][13] and Musu Dan in North Korea. The coldest months are January and February with the average air temperature of −20 °C (−4 °F) in the north and 5 °C (41 °F) in the south. The amplitude however increases to 2.3–2.8 m (7.5–9.2 ft) toward the north of the Strait of Tartary due to its funnel-like shape. A branch of the Kuroshio (Japan Current), the Tsushima Current, together with its northern branch, the East Korea Warm Current, flows north, bringing warmer and more saline water before flowing into the Pacific through the Tsugaru Strait as the Tsugaru Current, as well as into the Sea of Okhotsk through the La Perouse Strait as the Sōya Current. Its water balance is mostly determined by the inflow and outflow through the straits connecting it to the neighboring seas and the Pacific Ocean. There they merge into the Tsugaru Current and flow into the Pacific Ocean through the Tsugaru Strait. [27], Fishery had long been the main economic activity on the Sea of Japan. Tsunami waves were also recorded in the sea. The lights of South Korean cities and fishing boats on the Sea of Japan and the Yellow Sea are pictured as the International Space Station orbited 260 miles in altitude off the coast of Japan. It defines the geography of nations, and even more colors the very cultures and character of the people living along its shores or in the mountains towering above it. The sea is separated into three underwater basins, the Japan Basin, the Yamato Basin, and the Tsushima Basin. Winter temperatures are 0 °C (32 °F) or below in the north and 10–14 °C (50–57 °F) in the south. The temperature would sharply drop to 4 °C (39 °F) at 50 m (160 ft), then slowly decrease to 1 °C (34 °F) at 250 m (820 ft) and remain so down to the seabed. Nowadays the Sea of Japan is bounded by the Russian mainland and Sakhalin island to the north, the Korean Peninsula to the west, and the Japanese islands of Hokkaidō, Honshū and Kyūshū to the east and south. Max. Due to its inclusion by these land masses, it has practically no tide changes. Bottom deposits in the Sea of Japan indicate that sediments of continental origin, such as mud, sand, gravel, and fragments of rock, exist down to depths of some 650 to 1,000 feet (200 to 300 metres); hemipelagic sediments (i.e., half of oceanic origin), mainly consisting of blue mud rich in organic matter, are found down to depths of about 1,000 to 2,600 feet (300 to 800 metres); and deeper pelagic sediments, consisting of red mud, are found down to the sea’s greatest depths. A line running from Nagoya Saki (130°49′,5 E) in Kyûsyû through the islands of Uma Sima and Muture Sima (33°58′,5 N) to Murasaki Hana (34°01′ N) in Honsyû. It is bounded by Japan and Sakhalin Island to the east and by Russia and Korea on the Asian mainland to the west. The Island Nation stretches from the Sea of Okhotsk in the north to the East China Sea in the south. Omissions? Their formation had interrupted the migration of elephants into the Japanese islands at the end of the Neogene Period (about 2.6 million years ago). The Sea of Japan was a landlocked sea when the land bridge of East Asia existed circa 18,000 BCE. Updates? The Japanese government supports the exclusive use of the name "Sea of Japan" (日本海), while South Korea supports the alternative name "East Sea" (Korean: 동해; Hanja: 東海), and North Korea supports th… Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure from the Pacific Ocean. On the East. The intensity of shipments across the sea has been moderate owing to political issues, but it is steadily increasing as a result of the growth of East Asian economies. Japan strongly opposes unfounded arguments concerning the name “Sea of Japan,” and is calling for a better understanding of the issue and support for Japan’s position from the international community in order to maintain the sole use of the name, “Sea of Japan”. The sea is called Rìběn hǎi (日本海, literally "Japan Sea") or originally Jīng hǎi (鲸海, literally "Whale Sea") in China,[2] Yaponskoye more (Японское море, literally "Japanese Sea") in Russia, Chosŏn Tonghae (조선동해, literally "Korean East Sea") in North Korea, and Donghae (동해, literally "East Sea") in South Korea. It is located in the Northern and Eastern hemispheres of the Earth. Peter the Great Bay, Russian Zaliv Petra Velikogo, inlet, Sea of Japan, northwestern Pacific Ocean, in the Maritime (Primorye) region of far eastern Russia.The bay extends for 115 miles (185 km) from the mouth of the Tumen River (on the Russian-Chinese border) northeast across to Cape Povorotny. A typical variation of salinity across the sea in summer is 31.5‰ to 34.5‰ from north to south. [30] The Sea of Japan meets these conditions as it has frequent winds and cloudy skies, as well as compact, tall islands such as Rishiri (1,721 m or 5,646 ft), Ulleungdo (984 m or 3,228 ft) and Ōshima (732 m or 2,402 ft). [28] The average water density is 1.0270 g/cm3 in the north and 1.0255 g/cm3 in the south in winter. Associate Professor of Geography, University of Hawaii at Manoa, Honolulu. There are no large islands in the sea. The banks lying off the coasts of Japan are divided into groups, which include Okujiri Ridge, Sado Ridge, Hakusan Banks, Wakasa Ridge, and Oki Ridge. The hydrological isolation of the Sea of Japan also results in slightly lower average water salinity (34.09‰, where ‰ means parts per thousand) compared with the Pacific Ocean. The deepest, and thus the last to close, is the western channel of the Korea Strait. As world sea level dropped during the advance of the last Ice Age, the exit straits of the Sea of Japan one by one dried and closed. It can be divided into three basins: The Northern Japan basin is the deepest area of the Yamato basin lies … The sea has no large islands, bays or capes. This combination results in strong evaporation, which is especially noticeable between October and March when the strong (12–15 m/s [39–49 ft/s] or higher) north-western monsoon wind brings cold and dry continental air. Geophysical investigation has revealed that, while the ridge is of continental origin, the Japan Basin and the Yamato Basin are of oceanic origin. Along the coast of the Asian mainland three cold currents—the Liman, North Korea, and Central (or Mid-) Japan Sea cold currents—bring cooler, relatively fresh water southward. Walking Tour Video: Noto Peninsula, MITSUKEJIMA ISLAND In Japan (2020) Video November 22, 2020 boomersdaily Leave a comment. Fukuoka N. (1966). [28], The sea has a surface area of about 978,000 km2 (378,000 sq mi), a mean depth of 1,752 m (5,748 ft) and a maximum depth of 3,742 m (12,277 ft). This isolation also affects faunal diversity and salinity, both of which are lower than in the open ocean. Very few rivers empty into it, and their water amounts to less than one percent of the sea’s content. Schmidt in 1903–1904. In 1796, a British naval officer, William Robert Broughton explored the Strait of Tartary, the eastern coast of the Russian Far East and the Korean Peninsula. It depicts the area around the East Sea, including the Korean Peninsula, the mainland north of it, and the Japanese archipelago. Russian expeditions were made in 1853–1854 and 1886–1889 to measure the surface temperatures and record the tides. From the extremity of Siriya Saki (141°28′ E) to the extremity of Esan Saki (41°48′ N). The structure of the Sea of Japan can be divided into two layers: the surface water layer is about 300 meters deep, and the deep sea layer is below this. This cold layer at about 1,000 m (3,300 ft) is formed by sinking of cold water in the northern part of the sea in winter and is brought south by the sea currents; it is rather stable and is observed all through the year.[12][28]. 995x983 / 590 Kb Go to Map. However, in central-southern parts, it may be 8–10 °C (46–50 °F) down to 100–150 m (330–490 ft), 2–4 °C (36–39 °F) at 200–250 m (660–820 ft), 1.0–1.5 °C (33.8–34.7 °F) at 400–500 m (1,300–1,600 ft) and then remain at about 0 °C (32 °F) until the bottom. The Japanese archipelago separates the sea from the Pacific Ocean. The incursion of the Chinese in this region has intensified local tensions. Squid is mostly caught near the sea center and salmon near the northern and south-western shores. Sea of Japan - Sea of Japan - Economic aspects: Fisheries and mineral deposits form the main economic resources of the Sea of Japan. [5], The primary issue in the dispute revolves around a disagreement about when the name "Sea of Japan" became the international standard. On the contrary, the temperature in the south could gradually decrease to 6 °C (43 °F) at 200 m (660 ft), then to 2 °C (36 °F) at 260 m (850 ft) and to 0.04–0.14 °C (32.07–32.25 °F) at 1,000–1,500 m (3,300–4,900 ft), but then it would rise to about 0.3 °C (32.5 °F) near the bottom. Sea water has an average temperature of 17°C with the sea of Japan being a little below that (assuming 10 for now). The Sea of Japan was considered to be a frozen inner lake because of the lack of the warm Tsushima Current. Coordinates: .mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}40°N 135°E / 40°N 135°E / 40; 135. Tag Archives: Sea of Japan Travel, Videos. Sea water has an average temperature of 17°C with the sea of Japan being a little below that (assuming 10 for now). Coined as ‘Snow Country’ by the Nobel Prize-winning novelist Yasunari Kawabata, this prefecture’s slender stretch of land along Japan’s northern coast attracts some of the heaviest snowfall in the country. Because it is almost completely closed off from the Pacific Ocean it has almost no tidal activity and it also has lower salinity than the ocean. The Japanese scientific studies of the sea began only in 1915 and became systematic since the 1920s. Pelagic (oceanic) fishes include mackerel, horse mackerel, sardines, anchovies, herring, fishes of the salmon and trout family, sea bream, and squid; the demersal (sea-bottom) category includes cod, Alaskan pollack (bluefish), and Atka mackerel. This marginal sea is bordered by the countries South Korea, North Korea, Russia, and Japan. The middle water’s origin is in the intermediate water layers of the Kuroshio off the coast of Kyushu that enter the Sea of Japan via the Tsushima Current during the winter and spring. A dispute exists over the international name for the body of water which is bordered by Japan, Korea (North and South) and Russia. Thawing of ice in spring reduces water salinity in the north, but it remains high at 34.60–34.70‰ in the south, partly because of the inflow of salty water through the Korea Strait. They also feed the Sōya Current and exit through the La Perouse Strait to the Sea of Okhotsk. So add another ~4e21 kJ to the bill. Northern Sea of Japan Coast The Sea of Japan is the marginal sea between the Japanese archipelago, Sakhalin, the Korean Peninsula, and the Russia mainland. It measures 2,255 km from north to south and has a maximum width of about 1,070 km. [12] All the straits are rather shallow with a minimal depth of the order of 100 meters or less. Every two years since 1994 when Sea Japan was born in Yokohama, Japan’s shipbuilding and shipping industry gathers together at Sea Japan to showcase the very latest in marine technology and to meet and do business with their partners and suppliers from around the world. Sea of Japan, Japanese Nihon-kai, Russian Yaponskoye More, also called East Sea, Korean Tonghae or Donghae, marginal sea of the western Pacific Ocean. [28], There are three distinct continental shelves in the northern part (above 44° N). [12] There is also a well-developed seaweed production. Search for articles. The Defense Ministry said the two Su-34 jets, each with a crew of two, collided while maneuvering and went down 35 kilometers (22 miles) from the shore. The Name East Sea Used for Two Millennia. Oil Reserves B. Icebergs in water C. Fishing Area D. Mineral Water. [28] Most water (97% or 52,200 km3 [12,500 cu mi]) flows into the sea through the Korea Strait and discharges through the Tsugaru (64% or 34,610 km3 [8,300 cu mi], La Pérouse 10,380 km3 [2,490 cu mi]) and Korea straits. Mixed tides occur in Peter the Great Gulf and Korea strait. This winter monsoon brings typhoons and storms with the waves reaching 8–10 m (26–33 ft) which erode the western coasts of Japan. Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure from the Pacific Ocean. Of Esan Saki ( 41°48′ N ) separation from the Pacific Ocean scientific studies of the of. Print: Corrections due to its nearly separation from the Pacific Ocean Pacific. 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