2017
DOI: 10.17576/jsm-2017-4601-04
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Representing Landslides as Polygon (Areal) or Points? How Different Data Types Influence the Accuracy of Landslide Susceptibility Maps

Abstract: In the literatures, discussions on the accuracy of different models for landslide analysis have been discussed widely. However, to date, arguments on the type of input data (landslides in the form of point or polygon) and how they affect the accuracy of these models can hardly be found. This study assesses how different types of data (point or polygon) applied to the same model influence the accuracy of the model in determining areas susceptible to landsliding. A total of 137 landslides was digitised as polygo… Show more

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Cited by 11 publications
(12 citation statements)
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“…The landslide inventory is used to store the data on the landslides, in precise the location and areal extent of each landslide (Simon et al 2017). A total of 178 aerial photographs were used to map landslides with the scale of 1:12 000 throughout three assessment years, starting from 1984, 2009 and 2012.…”
Section: Methodsmentioning
confidence: 99%
“…The landslide inventory is used to store the data on the landslides, in precise the location and areal extent of each landslide (Simon et al 2017). A total of 178 aerial photographs were used to map landslides with the scale of 1:12 000 throughout three assessment years, starting from 1984, 2009 and 2012.…”
Section: Methodsmentioning
confidence: 99%
“…Pourghasemi et al, 2014 <1,500, 1,500-2,000, 2,000-2,500, 2,500-3,000, 3,000-3,500, >3,500 500 Pourtaghi et al, 2014<100, 100-500, 500-1000, 1000-1500, 1500-2000, 2000-2500, 2500-3000, 3000 m 500 Pradhan and Kim, 2017<75, 75-100, 100-150, 150-200, 200-250, >250 yok Pradhan et al, 20140-20, 20-25, 25-35, 35-65, 65-115, 115-252, 252-465, 465-705, 705-950, 950-2,000 yok Raja et al, 2017<50, 50-100, 100-150, 150-200, >200 50 Rozos et al, 2010<250, 250-500, 501-800, 801-1200, >1200 yok Saadatkhah et al, 20140-50, 50-100, 100-200, 200-300, >300 yok Sadr et al, 20140-100, 100-200, 200-300, 300-425 100 Shrestha et al, 2017<1281, 1281-1755, 1755-2254, 2254 yok Simon et al, 2017<30, 30-60, 60-90, >90 30 Tazik et al, 2014500-1000, 1000-1500, 1500-2000, >2000 500 Tsangaratos and Ilia, 2016<400, 401-600, 601-800, >801 200 Umar et al, 0-9.01, 9.01-18.02, 18.02-45.07, 45.07-90.14, 90.14-135,21, 135.21-198.31, 198.31-297.45, 297.46-458.73, 468.73-748.18, 748.18-2298 yok Wang et al, 20-850, 850-1000, 1000-1150, 1150-1300, 1300-1560yok...…”
Section: Researcher (S) /Yearmentioning
confidence: 99%
“…Atmosfera bumi terdiri daripada beberapa lapisan bermula daripada lapisan troposfera sehingga ke termosfera. Terdapat pelbagai kajian telah dijalankan untuk menyelidik lapisan atmosfera ini (Shojanoori et al 2016;Simon et al 2017). Namun begitu, penyelidikan ini memfokuskan pada lapisan ionosfera.…”
Section: Pengenalanunclassified