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Liyue represents the China-inspired region in Genshin Impact. The Geo-elemental nation is located in the eastern part of Teyvat and is the oldest established nation on the continent. [1] According to the lore, about 3,700 years ago, Rex Lapis founded Liyue. [2] The goddess Guizhong guarded Mt. Tianheng and built the Guizhong Ballista. [3]
A lee trough, also known as a dynamic trough, is "A pressure trough formed on the lee side of a mountain range in situations where the wind is blowing with a substantial component across the mountain ridge; often seen on United States weather maps east of the Rocky Mountains, and sometimes east of the Appalachians, where it is less pronounced."
The player may freely explore an open-world map. Here Aether, the male Traveler, is seen gliding, but the player can switch to other party members. Genshin Impact is an open-world, action role-playing game that allows the player to control one of four interchangeable characters in a party. [4]
A col, also called saddle point or neutral point, is in meteorology, the point of intersection of a trough and a ridge in the pressure pattern of a weather map. It takes the form of a saddle where the air pressure is relatively higher than that of the low-pressure regions, but lower than that of the anticyclonic zones. [1]
MiHoYo Co., Ltd. [note 1] is a Chinese video game development and publishing company founded in 2012 and headquartered in Shanghai.The company is best known for developing the Honkai series, Tears of Themis, Genshin Impact, and Zenless Zone Zero.
The Drake Passage, between the southern tip of South America and Antarctic, is infamous as one of the most dangerous journeys on the planet. But why is it so rough – and how can you cross safely?
Reindeer live in the far northern regions of Europe, North America, and Asia.They enjoy colder climates like tundra and boreal forests. We can find them in northern countries, which include:
A tropical upper tropospheric trough (TUTT), also known as the mid-oceanic trough, [1] is a trough situated in the upper-level (at about 200 hPa) tropics. Its formation is usually caused by the intrusion of energy and wind from the mid-latitudes into the tropics. It can also develop from the inverted trough adjacent to an upper level anticyclone.
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