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{"references": ["Amatulli, G., McInerney, D., Sethi, T., Strobl, P., & Domisch, S. (2020). Geomorpho90m, empirical evaluation and accuracy assessment of global high-resolution geomorphometric layers. Scientific Data, 7(1), 1-18. https://doi.org/10.1038/s41597-020-0479-6", "Conrad, O., Bechtel, B., Bock, M., Dietrich, H., Fischer, E., Gerlitz, L., ... & B\u00f6hner, J. (2015). System for automated geoscientific analyses (SAGA) v. 2.1. 4. Geoscientific Model Development, 8(7), 1991-2007.", "Dubayah, R., Blair, J. B., Goetz, S., Fatoyinbo, L., Hansen, M., Healey, S., ... & Silva, C. (2020). The Global Ecosystem Dynamics Investigation: High-resolution laser ranging of the Earth's forests and topography. Science of remote sensing, 1, 100002. https://doi.org/10.1016/j.srs.2020.100002", "Grohmann, C. H. (2018). Evaluation of TanDEM-X DEMs on selected Brazilian sites: Comparison with SRTM, ASTER GDEM and ALOS AW3D30. Remote Sensing of Environment, 212, 121-133. https://doi.org/10.1016/j.rse.2018.04.043", "Neteler, M., & Mitasova, H. (2013). Open source GIS: a GRASS GIS approach (Vol. 689). Springer Science & Business Media.", "Uuemaa, E., Ahi, S., Montibeller, B., Muru, M., & Kmoch, A. (2020). Vertical Accuracy of Freely Available Global Digital Elevation Models (ASTER, AW3D30, MERIT, TanDEM-X, SRTM, and NASADEM). Remote Sensing, 12(21), 3482. https://doi.org/10.3390/rs12213482", "Yamazaki, D., Ikeshima, D., Sosa, J., Bates, P. D., Allen, G. H., & Pavelsky, T. M. (2019). MERIT Hydro: a high\u2010resolution global hydrography map based on latest topography dataset. Water Resources Research, 55(6), 5053-5073. https://doi.org/10.1029/2019WR024873"]}
Digital Terrain Model geomorphometry derivatives based on the DTM for Continental Europe using the EPSG:3035 projection system. Processed using SAGA GIS, GRASS 7 GIS and GDAL at 3 standard spatial resolutions: 30-m, 100-m and 250-m. Derivatives include: devmean = deviation from mean value derived using SAGA GIS, downlocal / down = downslope local and general curvature derived using SAGA GIS, hillshade = hillshading derived using using GDAL gdaldem functions, mnr = Module Melton Ruggedness Number derived using SAGA GIS, northerness/easterness = derived using GRASS 7 GIS, openp / openn = openness positive negative derived using SAGA GIS, slope = slope in percent derived using GDAL gdaldem functions, topidx = a topographic index (wetness index) derived using GRASS 7 GIS, tpi = Topographic Wetness Index derived using SAGA GIS, vbf = Multiresolution Index of Valley Bottom Flatness derived using SAGA GIS, Detailed processing steps can be found here. Read more about the processing steps here. Derivatives were chosen aiming to support soil and vegetation mapping projects. The slope.percent map at 30-m has been converted from 0-100% scale to 0-200% (Byte format) to help decrease the file size.
This work has received funding from the European Union's the Innovation and Networks Executive Agency (INEA) under Grant Agreement Connecting Europe Facility (CEF) Telecom project 2018-EU-IA-0095 (https://ec.europa.eu/inea/en/connecting-europe-facility/cef-telecom/2018-eu-ia-0095).
topographic wetness index, digital terrain model, Continental Europe, slope, geomorphometry
topographic wetness index, digital terrain model, Continental Europe, slope, geomorphometry
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