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Ya-Sin Yang, Hsin-Fu Yeh, Chia-Chi Huang and Hsin-Yu Chen
Owing to active orogenic movement and the monsoon climate, rainfall-induced landslide disasters often occur in Taiwan. Hence, hillslope hydrology and stability have received considerable research attention. However, it remains difficult to accurately est...
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Claudia Schepp, Bernd Diekkrüger and Mathias Becker
While interflow from the slopes can be crucial for water and nutrient availability in low-input farming systems in wetlands in East Africa, very little data exist on hillslope hydrology and associated nutrient transport in deeply weathered saprolites ove...
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Aleen Pertuz-Paz, Gaspar Monsalve, Juan Carlos Loaiza-Úsuga, José Humberto Caballero-Acosta, Laura Inés Agudelo-Vélez and Roy C. Sidle
Soil creep is common along the hillslopes of the tropical Andes of Colombia, where very heterogeneous soils develop on old debris flow deposits and are subjected to abundant rainfall with a bimodal annual regime. In particular, the western hillside of th...
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Morgan Fonley, Ricardo Mantilla and Rodica Curtu
The concept of doing hydrology backwards, introduced in the literature in the last decade, relies on the possibility to invert the equations relating streamflow fluctuations at the catchment outlet to estimated hydrological forcings throughout the basin....
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Benjamin B. Mirus, Michael D. Morphew and Joel B. Smith
Consistent relations between shallow landslide initiation and associated rainfall characteristics remain difficult to identify, due largely to the complex hydrological and geological processes causing slopes to be predisposed to failure and those process...
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Yvonne Smit, Martine J. Van der Ploeg and Adriaan J. Teuling
Understanding hillslope runoff response to intense rainfall is an important topic in hydrology, and is key to correct prediction of extreme stream flow, erosion and landslides. Although it is known that preferential flow processes activated by macropores...
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Sayjro Kossi Nouwakpo and Chi-hua Huang
Pág. 1197 - 1211
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Reuter, R. J. Bell, J. C.
Pág. 365 - 372
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