${session.getAttribute("locale")} 5 Responding to multiple climate-linked stressors in a remote island context: the example of Yadua Island, Fiji. Thu 27 Jun 2019 13:12:13 AEST ]]> Geomorphic hazards in south‐west Saudi Arabia: The human–environmental nexus Thu 14 Nov 2019 16:24:38 AEST ]]> Root biomechanical traits in a montane mediterranean forest watershed: Variations with species diversity and soil depth Fri 25 Oct 2019 10:08:44 AEST ]]> Hydrogeomorphic processes and scaling issues in the continuum from soil pedons to catchments Fri 18 Oct 2019 13:17:52 AEST ]]> A Comparison of Piezometric Response in Unchanneled Hillslope Hollows: Coastal Alaska and Japan Fri 14 Jun 2019 13:50:27 AEST ]]> Landslides and debris flows strike Kyushu, Japan Fri 14 Jun 2019 13:49:21 AEST ]]> Evaluating landslide damage during the 2004 Chuetsu earthquake, Niigata Japan Fri 14 Jun 2019 13:49:18 AEST ]]> Geo-disaster Prediction and Geo-hazard Mapping in Urban and Surrounding Areas Progress Report in FY 2006 Fri 14 Jun 2019 13:49:05 AEST ]]> Application of Decision Analysis to Forest Road Deactivation in Unstable Terrain Fri 14 Jun 2019 13:49:03 AEST ]]> Dynamic earth system and ecological controls of rainfall-initiated landslides Fri 14 Jun 2019 13:48:57 AEST ]]> Stream response to subsidence from underground coal mining in central Utah Fri 14 Jun 2019 13:48:17 AEST ]]> Hydrogeomorphic linkages of sediment transport in headwater streams, Maybeso Experimental Forest, southeast Alaska Fri 14 Jun 2019 13:48:13 AEST ]]> The characteristics of woody debris and sediment distribution in headwater streams, southeastern Alaska Fri 14 Jun 2019 13:47:18 AEST ]]> Turbidity-based sediment monitoring in northern Thailand: Hysteresis, variability, and uncertainty 2000μm. Hysteresis in the monthly Q-TSS relationship was generally clockwise over the course of the monsoon season, but infrequent large dry-season storms disrupted the pattern in some years. The large decrease in annual loads during the study was believed to be related to depletion of fine sediment delivered to the stream by several landslides occurring the year prior to the study. The study indicated the importance of monitoring Q and turbidity at fine resolutions (e.g., sub-hourly) to capture the TSS dynamics and to make accurate load estimations in this flashy headwater stream where hysteresis in the Q-TSS signature varied at several time scales.]]> Fri 14 Jun 2019 13:47:11 AEST ]]> Soil conditions in three recent landslides in Southeast Alaska Fri 14 Jun 2019 13:46:58 AEST ]]> Erosion processes in steep terrain - Truths, myths, and uncertainties related to forest management in Southeast Asia Fri 14 Jun 2019 13:46:54 AEST ]]> Characteristics of landslides in unwelded pyroclastic flow deposits, southern Kyushu, Japan 200 mm) storms that triggered landslides was much lower than for smaller (≤ 200 mm) storms. Mean storm intensity and antecedent 7 day rainfall (API7) thresholds of > 5 mm h-1 and ≤ 30 mm (or API30 ≤ 60 mm), respectively, were useful to identify landslides triggered by rapid pore water pressure response, especially for shorter (< 20 h) duration events. During smaller storms with lower intensity, landslides are likely affected by a combined increase in soil weight and loss of suction when API30 ≥ 150 mm; simulations indicated that these weight and suction changes due to rainfall accumulation decreased factor of safety in steep Shirasu slopes, but did not necessarily trigger the landslides. All but two of the 21 landslides that plotted below a general rainfall intensity-duration threshold for landslide initiation had API30 values > 235 mm, indicating that they were highly influenced by the combined effects of the accumulated weight of rainfall and loss of suction. Our findings show that both event rainfall characteristics and antecedent conditions affect the hydrogeomorphic processes that trigger different types of landslides in Shirasu. This knowledge and the thresholds we have identified are useful for predicting the occurrence of different types of landslides in Shirasu deposits and improving sediment disaster prevention practices, including real-time warning systems.]]> Fri 14 Jun 2019 13:46:52 AEST ]]> Vadose zone process that control landslide initiation and debris flow propagation Fri 14 Jun 2019 13:46:38 AEST ]]> Mass Movement Fri 14 Jun 2019 13:46:31 AEST ]]> Pore water pressure assessment in a forest watershed: Simulations and distributed field measurements related to forest practices Fri 14 Jun 2019 13:46:24 AEST ]]> Internal erosion during soil pipeflow: State of the science for experimental and numerical analysis Fri 14 Jun 2019 13:45:58 AEST ]]> The dilemma of mountain roads Fri 14 Jun 2019 13:45:44 AEST ]]> The influence of plant root systems on subsurface flow: Implications for slope stability Fri 14 Jun 2019 13:45:31 AEST ]]> Ecosystem changes following the 2016 Kumamoto earthquakes in Japan: Future perspectives Fri 14 Jun 2019 13:45:25 AEST ]]>