Traditional Culture Encyclopedia - Weather forecast - What is the sea near Dalian?

What is the sea near Dalian?

Dalian is close to the Yellow Sea and Bohai Sea. Dalian is located at the junction of the Yellow Sea and the Bohai Sea. Among them, the main rivers flowing into the Yellow Sea in Dalian are Biliu River, Naying River, Zhuanghe River and Zanzi River, and the main rivers flowing into Bohai Sea are Fuzhou River, Liguancun River and Sanshilipu River.

Bohai Sea is the only inland sea in China, the northernmost sea off the coast of China and the shallowest semi-enclosed inland sea in China. Surrounded by the land of Liaoning, Hebei, Tianjin and Shandong provinces on three sides, it communicates with the Yellow Sea through the Bohai Strait.

The Yellow Sea is the largest marginal sea in the western Pacific Ocean, which lies between China and the Korean Peninsula. The northwest of the Yellow Sea is connected with the Bohai Sea through the Bohai Strait, the east is connected with the Korean Strait through the cheju strait, and the south is connected with the East China Sea from the Qidong corner on the northeast coast of the Yangtze River estuary to the southwest corner of Jeju Island.

Extended data:

1. Yellow Sea: In the northern part of the Yellow Sea, the line connecting China Penglai Tian Hengshan and China Dalian Laotieshan is the dividing line between China Yellow Sea and Bohai Sea. The main bays are China's West Korea Bay, Haizhou Bay and Jiaozhou Bay, which are connected with the Bohai Sea through cheju strait via the Korean Strait, Ma Haixia and the Sea of Japan.

2. Bohai Sea: The Bohai Sea consists of Liaodong Bay, Bohai Bay, Laizhou Bay and the central basin. The main rivers entering the sea are the Yellow River, Liaohe River, Luanhe River and Haihe River, with an annual runoff of 88.8 billion cubic meters. The terrain inclines from the coast to the middle and the strait, and the terrain is monotonous and gentle. There are traces of ancient coastlines and ancient rivers on the seabed. Bohai Sea is a Mesozoic-Cenozoic subsidence basin with Precambrian metamorphic rocks as its basement.

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