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High Water

   Also found in: Dictionary/thesaurus, Acronyms, Wikipedia 0.02 sec.
high water [′hī ¦wȯd·ər]
(oceanography)

High Water 

the relatively prolonged and significant rise in the water level of a river; it occurs each year at the same season. High water is usually associated with the overflowing of the channel and flooding of the floodplain. It is caused by prolonged, intensified influx of water from the spring melting of snow on plains, the summer thawing of snow and glaciers in mountains, or heavy seasonal rains (for example, related to summer monsoons). High water caused by the spring thaw is typical for rivers that flow through plains. They include rivers in which spring runoff is predominant (for example, the Volga and Ural) and rivers in which summer runoff is greater (for example, the Anadyr’, Yukon, and Mackenzie). High water caused by summer thawing of mountain snow and ice is typical of the rivers of Middle Asia, the Caucasus, and the Alps. High water caused by summer monsoonal rains characterizes the rivers of Southeast Asia (for example, the Yangtze and Mekong).



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In low water these neat narrow-edged dikes project four or five inches above the surface, like the comb of a submerged roof, but in high water they are overflowed.
Having thus fixed fifty hooks to as many cables, I went back to the north-east coast, and putting off my coat, shoes, and stockings, walked into the sea, in my leathern jerkin, about half an hour before high water.
The flat intermediate country was intersected by a labyrinth of tidal streams, winding up from the invisible sea in strange fantastic curves -- rivers at high water, and channels of mud at low.
 
 
 
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