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Slushflows: basic properties and spreadingстатья
Информация о цитировании статьи получена из
Scopus
Дата последнего поиска статьи во внешних источниках: 28 мая 2015 г.
- Автор: Perov V.F.
- Журнал: Publikasjon - Norges Geotekniske Institutt
- Номер: 203
- Год издания: 1998
- Первая страница: 203
- Последняя страница: 209
- Аннотация: The article presents results of an analytical review of factual data and scientific studies concerning slushflows. The basic conditions and gears of origin, parameters and typology of flows are considered, as well as the impact slushflows have upon topography and vegetation, spreading and seasonal distribution, dangerous consequences of snowslides. Slushflows are regarded as zonal paragenic mudflow phenomena typical of the subarctic climate zone. The area of territories with slushflows predominance accounts for 20 per cent of the total land subject to mudflow phenomena. Recurrence intervals of snowslides average one in 5 to 10 years. The article presents results of an analytical review of factual data and scientific studies concerning slushflows. The basic conditions and gears of origin, parameters and typology of flows are considered, as well as the impact slushflows have upon topography and vegetation, spreading and seasonal distribution, dangerous consequences of snowslides. Slushflows are regarded as zonal paragenic mudflow phenomena typical of the subarctic climate zone. The area of territories with slushflows predominance accounts for 20 per cent of the total land subject to mudflow phenomena. Recurrence intervals of snowslides average one in 5 to 10 years.
- Добавил в систему: Сократов Сергей Альфредович