2015
DOI: 10.1007/s10346-015-0626-x
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Shallow landslide susceptibility mapping using high-resolution topography for areas devastated by super typhoon Haiyan

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Cited by 16 publications
(13 citation statements)
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“…J. Zhang, van Meerveld, et al, ) were used in regression equations linking the Basper gauge to the respective gauges at Manobo ( R 2 = 0.85–0.88) to estimate P at Manobo. No corrections were made for wind‐related underestimation of P because wind speeds (as measured at the Basper weather station) were generally low and the application of correction methods (e.g., Førland et al, ) for the extreme wind speeds encountered during the Haiyan event (Rabonza et al, ) would have led to unverifiable and uncertain corrections. Instead, a recording cylindrical fog gauge placed at the Basper station that has a 100% catch efficiency for near‐horizontal wind‐driven rain (Frumau et al, ) was used to estimate extra inputs of near‐horizontal wind‐driven rainfall during the Haiyan event.…”
Section: Methodsmentioning
confidence: 99%
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“…J. Zhang, van Meerveld, et al, ) were used in regression equations linking the Basper gauge to the respective gauges at Manobo ( R 2 = 0.85–0.88) to estimate P at Manobo. No corrections were made for wind‐related underestimation of P because wind speeds (as measured at the Basper weather station) were generally low and the application of correction methods (e.g., Førland et al, ) for the extreme wind speeds encountered during the Haiyan event (Rabonza et al, ) would have led to unverifiable and uncertain corrections. Instead, a recording cylindrical fog gauge placed at the Basper station that has a 100% catch efficiency for near‐horizontal wind‐driven rain (Frumau et al, ) was used to estimate extra inputs of near‐horizontal wind‐driven rainfall during the Haiyan event.…”
Section: Methodsmentioning
confidence: 99%
“…and 11 km from Manobo). Average monthly wind speeds at Tacloban airport vary between 1.5 and 2.4 m s −1 but can be very high during typhoon events (Rabonza et al, ). Average daily reference evaporation ET 0 (Allen, Pereira, Raes, & Smith, ) calculated using basic climatic data for Tacloban Airport ranges between 3.0 (December) and 4.8 mm day −1 (April), with an annual total of 1,385 mm.…”
Section: Study Areamentioning
confidence: 99%
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“…Sarkar et al 2016;Aristizábal et al 2015;Teixeira et al 2015). The D∞ algorithm has been used as an input for the calculation of landslide susceptibility via the application of the SINMAP model (i. e. Arkgun and Erkan 2016; Rabonza et al 2016;Nery and Vieira 2015).…”
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confidence: 99%