「潮瀬戸」に関連した英語例文の一覧と使い方 - Weblio英語例文検索

瀬戸内海の海流は満潮時に豊後水道や紀伊水道から瀬戸内海に流れ込み瀬戸内海のほぼ中央に位置する鞆の浦沖でぶつかり、逆に干潮時には鞆の浦沖を境にして東西に分かれて流れ出してゆく。例文帳に追加

At high tide, the ocean currents from the Bungo-suido Channel and the Kii-suido Channel flow into the Seto Inland Sea, where they collide off the coast of Tomonoura (located roughly in the center of the Seto Inland Sea); at low tide, however, they flow away from each other, with the current from the Kii-suido Channel flowing to the east and that from the Bungo-suido Channel flowing to the west and the coast of Tomonoura serving as a kind of central border.  - Wikipedia日英京都関連文書対訳コーパス

海上保安庁の潮流の調査に基づいても、合戦の行われた早鞆瀬戸より東側の海域では1ノット以下という結果が出ている。例文帳に追加

A study conducted by the Japan Coast Guard also found that the current in the area east of the Kanmon straits, where the battle was fought, was under one knot.  - Wikipedia日英京都関連文書対訳コーパス

「地乗り」と呼ばれる陸地を目印とした沿岸航海が主流の時代に、沼隈半島沖の瀬戸内海を横断するには鞆の浦で潮流が変わるのを待たなければならなかった。例文帳に追加

During the period when a near-coasted voyage using the geonavigation called 'Jinori' was the mainstream, people had to wait for the changing tide at Tomonoura to sail across the Seto Inland Sea off the Numakuma Peninsula.  - Wikipedia日英京都関連文書対訳コーパス

一　身網の設置される場所の最深部が最高潮時において水深二十七メートル（沖縄県にあつては、十五メートル）以上であるもの（瀬戸内海（第百十条第二項に規定する瀬戸内海をいう。）におけるます網漁業並びに陸奥湾（青森県焼山崎から同県明神崎灯台に至る直線及び陸岸によつて囲まれた海面をいう。）における落とし網漁業及びます網漁業を除く。）例文帳に追加

(i) A fishery in which the deepest water depth at the place where the body of a fishing net is fixed is 27 meters (15 meters in Okinawa Prefecture) or more at the time of the highest sea level (excluding the fishery using a pound net with some cube-shaped bags in the Seto Inland Sea (the Seto Inland Sea provided in paragraph (2), Article 110) and the fishery using a fixed shore trap net with a pocket and the fishery using a pound net with some cube-shaped bags in the Mutsu Bay (the sea surrounded by the straight line between Yakeyamazaki, Aomori Prefecture and the lighthouse at Cape Myojingasaki, Aomori Prefecture and by the shore).  - 日本法令外国語訳データベースシステム

この黒板説については、近年になって反論が出され、海事史の金指正三博士は1990年に潮流のコンピュータ解析を行い、合戦の行われた日は小潮流の時期で、8ノットという早い潮流は無く、また大正時代に潮流を調査した場所は最も狭い早鞆瀬戸であり（ここで千艘以上の兵船で戦うことは不可能）、広い干珠島、満珠島辺りの海域では潮流は1ノット以下であり合戦に影響を与えるものではないとした。例文帳に追加

Concerning KUROITA's theory, in recent years objections to it have surfaced; in 1990 the maritime historian Dr. Shozo KANASASHI ran a computer analysis of the tides on the day of the battle, and concluded that there was a neap tide that day, and thus that there could not have been a strong, swift current of eight knots, and moreover pointed out that the tidal study done in the Taisho period had been conducted at the narrowest point of the Kanmon straits (where it would have been impossible for more than 1000 ships to fight), concluding that in the spacious area of sea near Kanju and Manju islands, the tide was under one knot in speed and would have had no influence over the course of the battle.  - Wikipedia日英京都関連文書対訳コーパス