Abstract
The requirements of the debris flows’ parameters assessments vary from country to country. They are based on different theoretical and empirical constructions and are validated by data from different regions. This makes difficult comparison of the reported results on estimated debris flows activity and extent. The Russian normative documents for the debris flows’ parameters calculations are based on empirically-measured parameters in wide range of geological and climatic conditions at the territory of former USSR, but still not cover all the possible conditions of debris flow formation. An attempt was made to check applicability of the Russian empirical constructions for the conditions of the debris flows formation in Yunnan, China, where unique long-term dataset of debris flows characteristics is collected by the Dongchuan Debris Flow Observation and Research Station. The results show, that in general the accepted in Russia methodology of calculation of the parameters of debris flows of certain probability corresponded well to the observed in Dongchuan debris flows characteristics. Some discrepancies (in the average debris flow depth) can be explained by unknown exact return period of the actually observed debris flows. This allowed to conclude that the presently adopted empirical dependencies based on country-wide (USSR) empirical data can be extrapolated up to the monsoon climate and geological conditions of Yunnan province.
Highlights
The study of debris flow activity in China has longstanding history
Studies of debris flows at the Dongchuan Debris Flow Observation and Research Station have shown, that the main genetic type of debris flows in the Jiangjia Ravine are rain debris flows, the origination of which corresponds with a period of intense monsoon rains
The formation of landslide dams and their subsequent breaching and rapid erosion can lead to the formation of debris flows
Summary
The study of debris flow activity in China has longstanding history. Research is actively conducted in such provinces as Sichuan, Yunnan, Gansu, Shaanxi, etc. In 1961, a unique Dongchuan Debris Flow Observation and Research Station (DDFORS) was organized in the north of Yunnan province. The station is positioned in the valley of the Jiangjia creek and is the right-hand tributary of the larger river Xiaojiang, being part of the Upper Yangtze River basin. Continuous year-round observations have been conducted at this station with automatic fixation of the main parameters of debris flows since 1987 (Fig. 1). Since 2000, the station was authorized to be the State Key Field Observation Station
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