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dc.contributor.authorPANAGOS Panagiotisen_GB
dc.contributor.authorBALLABIO CRISTIANOen_GB
dc.contributor.authorBORRELLI PASQUALEen_GB
dc.contributor.authorMEUSBURGER Katrinen_GB
dc.date.accessioned2015-10-16T00:14:31Z-
dc.date.available2015-10-14en_GB
dc.date.available2015-10-16T00:14:31Z-
dc.date.created2015-10-14en_GB
dc.date.issued2016en_GB
dc.date.submitted2014-09-24en_GB
dc.identifier.citationCATENA vol. 137 p. 161-172en_GB
dc.identifier.issn0341-8162en_GB
dc.identifier.urihttp://www.sciencedirect.com/science/article/pii/S0341816215301156en_GB
dc.identifier.urihttp://publications.jrc.ec.europa.eu/repository/handle/JRC91862-
dc.description.abstractRainfall erosivity considers the effects of rainfall amount and intensity on soil detachment. Rainfall erosivity is most commonly expressed as the R-factor in the Universal Soil Loss Equation (USLE) and its revised version, RUSLE. Several studies focus on spatial analysis of rainfall erosivity ignoring the intra-annual variability of this factor. This study assesses rainfall erosivity in Greece on a monthly basis in the form of the RUSLE R-factor, based on a 30-min data from 80 precipitation stations covering an average period of almost 30 years. The spatial interpolation was done through a Generalised Additive Model (GAM). The observed intra-annual variability of rainfall erosivity proved to be high. Thewarmseason is 3 times less erosive than the cold one. November, December and October are the most erosive months contrary to July, August and May which are the least erosive. The proportion between rainfall erosivity and precipitation, expressed as erosivity density, varies throughout the year. Erosivity density is lowin the first 5 months (January–May) and is relatively high in the remaining 7 months (June–December) of the year. The R-factor maps reveal also a high spatial variability with elevated values in the western Greece and Peloponnesus and very lowvalues inWestern Macedonia, Thessaly, Attica and Cyclades. The East–West gradient of rainfall erosivity differs per month with a smoother distribution in summer and a more pronounced gradient during the winter months. The aggregated data for the 12 months result in an average Rfactor of 807 MJ mmha−1 h−1 year−1 with a range from 84 to 2825 MJmmha−1 h−1 year−1. The combination of monthly R-factor maps with vegetation coverage and tillage maps contributes to better monitor soil erosion risk at national level and monthly basis.en_GB
dc.description.sponsorshipJRC.H.5-Land Resources Managementen_GB
dc.format.mediumPrinteden_GB
dc.languageENGen_GB
dc.publisherELSEVIER SCIENCE BVen_GB
dc.relation.ispartofseriesJRC91862en_GB
dc.titleSpatio-temporal analysis of rainfall erosivity and erosivity density in Greeceen_GB
dc.typeArticles in periodicals and booksen_GB
dc.identifier.doi10.1016/j.catena.2015.09.015en_GB
JRC Directorate:Sustainable Resources

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