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Dynamics of the Ice Cover and Peculiarities of the Ice Transportation of the Sediments at the Tidal Flats of the Kandalaksha Gulf of the White Seaстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 5 июня 2019 г.
- Авторы: Romanenko F.A., Repkina T.Yu, Efimova L.E., Bulochnikova A.S.
- Журнал: Oceanology
- Том: 52
- Номер: 5
- Год издания: 2012
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 710
- Последняя страница: 720
- DOI: 10.1134/S000143701205013X
- Аннотация: Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, mor phology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone’s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains finesandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice’s spreading by 4–6 times in the warm years and 2–4 times in the cold years, several thousand tons of sediments mostly from the tidal flat’s surface (100–700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area.
- Добавил в систему: Романенко Фёдор Александрович