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- W2201723888 abstract "Extreme rainfall events, seasonal weather extremes and long term climate change present a threat to the stability of natural and engineered slopes by altering slope hydrology and shear strength beyond recent historical values. The temporal and spatial fluctuation of slope wetting and drying in response to weather event sequences can be represented using a surface water balance approach of rainfall infiltration and potential evapotranspiration, such as a soil moisture deficit calculation (SMD). This provides an opportunity to address the regional susceptibility of slopes to become unstable when exposed to adverse weather event sequences. However, case studies have shown that site specific characterisation of foundation geology (e.g. permeability and shear strength) is required to assess the vulnerability of specific slopes to pore water pressure fluctuations and slope failure during extreme weather events. The relationship between underlying geology and landslide incidence during extreme weather extremes is illustrated by comparing long term weather data, soil moisture deficit calculations and geological information using a database of over 400 UK land-slide events that occurred between 2004 and 2014." @default.
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- W2201723888 date "2015-09-13" @default.
- W2201723888 modified "2023-09-25" @default.
- W2201723888 title "The influence of slope geology on landslide occurrence during extreme rainfall" @default.
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