The drainage basin, river, and delta zone together constitute a complex open dipole system. In it, the watershed subsystem plays the role of an accumulator of high potential energy of water, the channel zones are cumulative transit zones of the potential energy of water, and the estuarine zones are dissipators of this energy, minimizing its level to the maximum. It is convenient to represent such a system as a “drainage” model, which allows us to consider all types of floods in its various sections and at the same time give a comparative assessment of the potential of river systems as dipole formations from tectonic positions.
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- Системология
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