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Mnogochislennye issledovaniya dinamiki vod v pribrezhnyh zonah morya otmechayut, chto vdol'beregovye struynye techeniya chasche formiruyutsya v usloviyah uzkogo shel'fa i rezkogo uklona dna. Suschestvovanie ustoychivogo struynogo techeniya igraet rol' zapirayuschego mehanizma dlya vynosa v otkrytoe more skaplivayuschihsya v pribrezhnoy zone vzveshennyh veschestv i samoochischeniya vodnoy ekosistemy. Vozniknovenie vihrevyh struktur s pribrezhnoy storony struynogo techeniya mozhet privodit' k ventilyacii pribrezhnyh vod cherez os' struynogo techeniya. Iz-za osobennostey donnoy i beregovoy topografii masshtaby takih vihrevyh struktur mogut umen'shat'sya do takoy stepeni, chto oni ne sposobny budut osuschestvlyat' ochistku pribrezhnyh vod vplot' do beregovoy linii.
FORMIROVANIE SUBMEZOMASShTABNYH VIHREY
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