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Forecast of avalanche danger for the intracontinental regions of northeast of Eurasiaстатья
Информация о цитировании статьи получена из
Scopus
Дата последнего поиска статьи во внешних источниках: 28 мая 2015 г.
- Авторы: Seliverstov Y.G., Glazovskaya T.G.
- Журнал: Publikasjon - Norges Geotekniske Institutt
- Номер: 203
- Год издания: 1998
- Первая страница: 245
- Последняя страница: 248
- Аннотация: The research area includes the Kolyma riverhead with tributaries. For this territory the extreme continental climate with very frost winters is common. The duration of snow cover is 200-230 days. The domination of low temperatures with small thickness of snow cover causes strong recrystallization of snow pack. On the other hand the intensity of this process often is not high. Significant loosening determines an unstable condition of snow on mountain slopes. Under certain conditions even the small increase of loading is capable to cause avalanching. The origin of the majority of avalanches (more than 60%) is connected with fresh snow fall on the friable base. A network of avalanche research and meteorological stations in this area is scarce. In such conditions only background (area) forecast is possible. At the creation of the forecast technique the analysis of large number of the factors of avalanching process in the region was carried out. The forecast includes computation and an expert estimation of snow-avalanche situation. The data of meteorological station Kulu, located at the center of area, are used as the basis of the technique. The sum of precipitation, its intensity, temperature of air and its change during the snowfall are distinguished as predictors. The final forecast and definition of possible places of crashing of avalanches occurs with the improvement of the data of other avalanche research and meteorological stations. The character of winter is also taken into account. The forecast is made on nearest 12 hours 2 times per day. It has an alternative character. The research area includes the Kolyma riverhead with tributaries. For this territory the extreme continental climate with very frost winters is common. The duration of snow cover is 200-230 days. The domination of low temperatures with small thickness of snow cover causes strong recrystallization of snow pack. On the other hand the intensity of this process often is not high. Significant loosening determines an unstable condition of snow on mountain slopes. Under certain conditions even the small increase of loading is capable to cause avalanching. The origin of the majority of avalanches (more than 60%) is connected with fresh snow fall on the friable base. A network of avalanche research and meteorological stations in this area is scarce. In such conditions only background (area) forecast is possible. At the creation of the forecast technique the analysis of large number of the factors of avalanching process in the region was carried out. The forecast includes computation and an expert estimation of snow-avalanche situation. The data of meteorological station Kulu, located at the center of area, are used as the basis of the technique. The sum of precipitation, its intensity, temperature of air and its change during the snowfall are distinguished as predictors. The final forecast and definition of possible places of crashing of avalanches occurs with the improvement of the data of other avalanche research and meteorological stations. The character of winter is also taken into account. The forecast is made on nearest 12 hours 2 times per day. It has an alternative character.
- Добавил в систему: Сократов Сергей Альфредович