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Write 15 pages with APA style on Water Depletion of Yellow River in China. The section also gives a detailed account of the Yellow river’s drying history. In particular, it gives the dates in which th
Write 15 pages with APA style on Water Depletion of Yellow River in China. The section also gives a detailed account of the Yellow river’s drying history. In particular, it gives the dates in which the river has dried up such as in 1972 and 1997.  .
The Yellow River remains of the most important river in Chinese history. Also referred to as Huanghe, Yellow River is among the largest Rivers in China. The river has its origins in the Bayangela Mountains that are found on the Western side of the country. The river traverses many areas including Gobi desert, Loess Plateau, and terminates in Bohai Gulf. In brief, the Yellow River cuts across over 9 Provinces and covers a total distance of 5,400 Km (Zhu, Giordano and Cai 2)
Despite the significance the river holds with regards to China’s political, economic, and social development, it is now faced with a threat of drying and flooding. These issues have at particular instances have caused misery to the Chinese people at scales almost unheard of elsewhere across the globe. The Yellow River’s characteristic of exhibiting two patterns in relation to human livelihood has led to its being called “the Cradle of Chinese civilization.”
Since the time the People’s Republic of China found its independence in 1949, major achievements have occurred with regards to flood control and, through development, drought mitigation in the Yellow River basin. Although the problems of flooding have always existed in the Yellow River. that the river started drying in the 1990s has caused concerns among the basin management and other environmentalists.
This is the largest part of the River and usually drains over half of the entire basin area (Giordano, Zhu, and Cai). The reach covers from where the river originates in the mountains to the Toudaoguai close to Datong city. Although the upper reach forms the largest part of the river’s basin surface, the contribution emanates largely from two distinct geographic backdrops that have a characteristic counteracting the physical process (Zhu et al. 17).
