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Landslide rates and hillslope turnover, Kosñipata Valley, Peru (Clark et al. 2016)

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Created: Feb 20, 2017 at 2:43 a.m.
Last updated: Feb 21, 2017 at 3:43 a.m.
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Please cite: Clark, K. E., West, A. J., Hilton, R. G., Asner, G. P., Quesada, C. A., Silman, M. R., Saatchi, S. S., Farfan Rios, W., Martin, R. E., Horwath, A. B., Halladay, K., New, M., and Malhi, Y. (2016), Storm-triggered landslides in the Peruvian Andes and implications for topography, carbon cycles, and biodiversity, Earth Surface Dynamics, 4, 47-70, doi: 10.5194/esurf-4-47-2016.

Landslide rates (Rls, %yr/1) calculated by 1 km2 grid cell in Figure 2b from Clark et al. (2016). In the table landslide rates appear as L_occurrence.

Hillslope turnover (tls, yr) rates calculated as the time for landslides, at the current measured rate (Rls), to impact 100% of each cell area in Figure 2c from Clark et al. (2016). In the table landslide derived hillslope turnover labelled as L_turnover.

Topographic shadow (http://www.hydroshare.org/resource/bdb9c4b4788d4141845947c81e5cceba) was removed from mapped landslides (http://dx.doi.org/10.4211/hs.90487bcf16e44c62a677ae33ef95e968) and then landslide rates were determined for a 1km2 grid.

This product was created by Kathryn Clark (kathryn.clark23@gmail.com).

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Resource Level Coverage


Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
North Latitude
East Longitude
South Latitude
West Longitude


How to Cite

Clark, K., J. West, R. Hilton (2017). Landslide rates and hillslope turnover, Kosñipata Valley, Peru (Clark et al. 2016), HydroShare, http://www.hydroshare.org/resource/147e9ebecde442ed97738de7f404c057

This resource is shared under the Creative Commons Attribution CC BY.



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