Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)

Rainfall erosivity exhibits a high spatiotemporal variability. Rain gauges are not capable of detecting small-scale erosive rainfall events comprehensively. Nonetheless, many operational instruments for assessing soil erosion risk, such as the erosion atlas used in the state of Hesse in Germany, are...

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Main Authors: Jennifer Kreklow, Bastian Steinhoff-Knopp, Klaus Friedrich, Björn Tetzlaff
Format: Article
Language:English
Published: MDPI AG 2020-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/5/1424
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spelling doaj-4d6e9640ada84909898e4b5e12b612332020-11-25T03:15:33ZengMDPI AGWater2073-44412020-05-01121424142410.3390/w12051424Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)Jennifer Kreklow0Bastian Steinhoff-Knopp1Klaus Friedrich2Björn Tetzlaff3Institute of Physical Geography and Landscape Ecology, Leibniz Universität Hannover, Schneiderberg 50, 30167 Hannover, GermanyInstitute of Physical Geography and Landscape Ecology, Leibniz Universität Hannover, Schneiderberg 50, 30167 Hannover, GermanyHessian Agency for Nature Conservation, Environment and Geology, 65203 Wiesbaden, GermanyInstitute of Bio- and Geosciences IBG-3, Forschungszentrum Jülich GmbH, 52425 Jülich, GermanyRainfall erosivity exhibits a high spatiotemporal variability. Rain gauges are not capable of detecting small-scale erosive rainfall events comprehensively. Nonetheless, many operational instruments for assessing soil erosion risk, such as the erosion atlas used in the state of Hesse in Germany, are still based on spatially interpolated rain gauge data and regression equations derived in the 1980s to estimate rainfall erosivity. Radar-based quantitative precipitation estimates with high spatiotemporal resolution are capable of mapping erosive rainfall comprehensively. In this study, radar climatology data with a spatiotemporal resolution of 1 km<sup>2</sup> and 5 min are used alongside rain gauge data to compare erosivity estimation methods used in erosion control practice. The aim is to assess the impacts of methodology, climate change and input data resolution, quality and spatial extent on the R-factor of the Universal Soil Loss Equation (USLE). Our results clearly show that R-factors have increased significantly due to climate change and that current R-factor maps need to be updated by using more recent and spatially distributed rainfall data. Radar climatology data show a high potential to improve rainfall erosivity estimations, but uncertainties regarding data quality and a need for further research on data correction approaches are becoming evident.https://www.mdpi.com/2073-4441/12/5/1424R-factorsoil erosionUSLErainfall intensitymodelingradar climatology
collection DOAJ
language English
format Article
sources DOAJ
author Jennifer Kreklow
Bastian Steinhoff-Knopp
Klaus Friedrich
Björn Tetzlaff
spellingShingle Jennifer Kreklow
Bastian Steinhoff-Knopp
Klaus Friedrich
Björn Tetzlaff
Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
Water
R-factor
soil erosion
USLE
rainfall intensity
modeling
radar climatology
author_facet Jennifer Kreklow
Bastian Steinhoff-Knopp
Klaus Friedrich
Björn Tetzlaff
author_sort Jennifer Kreklow
title Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
title_short Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
title_full Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
title_fullStr Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
title_full_unstemmed Comparing Rainfall Erosivity Estimation Methods Using Weather Radar Data for the State of Hesse (Germany)
title_sort comparing rainfall erosivity estimation methods using weather radar data for the state of hesse (germany)
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-05-01
description Rainfall erosivity exhibits a high spatiotemporal variability. Rain gauges are not capable of detecting small-scale erosive rainfall events comprehensively. Nonetheless, many operational instruments for assessing soil erosion risk, such as the erosion atlas used in the state of Hesse in Germany, are still based on spatially interpolated rain gauge data and regression equations derived in the 1980s to estimate rainfall erosivity. Radar-based quantitative precipitation estimates with high spatiotemporal resolution are capable of mapping erosive rainfall comprehensively. In this study, radar climatology data with a spatiotemporal resolution of 1 km<sup>2</sup> and 5 min are used alongside rain gauge data to compare erosivity estimation methods used in erosion control practice. The aim is to assess the impacts of methodology, climate change and input data resolution, quality and spatial extent on the R-factor of the Universal Soil Loss Equation (USLE). Our results clearly show that R-factors have increased significantly due to climate change and that current R-factor maps need to be updated by using more recent and spatially distributed rainfall data. Radar climatology data show a high potential to improve rainfall erosivity estimations, but uncertainties regarding data quality and a need for further research on data correction approaches are becoming evident.
topic R-factor
soil erosion
USLE
rainfall intensity
modeling
radar climatology
url https://www.mdpi.com/2073-4441/12/5/1424
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