CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran

Abstract Soil erosion (SE) and climate change are closely related to environmental challenges that influence human wellbeing. However, the potential impacts of both processes in semi-arid areas are difficult to be predicted because of atmospheric variations and non-sustainable land use management. T...

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Autores principales: Fatemeh Hateffard, Safwan Mohammed, Karam Alsafadi, Glory O. Enaruvbe, Ahmad Heidari, Hazem Ghassan Abdo, Jesús Rodrigo-Comino
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Publicado: Nature Portfolio 2021
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spelling oai:doaj.org-article:bd1bbdf84f944ecc9f652ec00bbbd71a2021-12-02T13:26:28ZCMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran10.1038/s41598-021-86618-z2045-2322https://doaj.org/article/bd1bbdf84f944ecc9f652ec00bbbd71a2021-03-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-86618-zhttps://doaj.org/toc/2045-2322Abstract Soil erosion (SE) and climate change are closely related to environmental challenges that influence human wellbeing. However, the potential impacts of both processes in semi-arid areas are difficult to be predicted because of atmospheric variations and non-sustainable land use management. Thus, models can be employed to estimate the potential effects of different climatic scenarios on environmental and human interactions. In this research, we present a novel study where changes in soil erosion by water in the central part of Iran under current and future climate scenarios are analyzed using the Climate Model Intercomparison Project-5 (CMIP5) under three Representative Concentration Pathway-RCP 2.6, 4.5 and 8.5 scenarios. Results showed that the estimated annual rate of SE in the study area in 2005, 2010, 2015 and 2019 averaged approximately 12.8 t ha−1 y−1. The rangeland areas registered the highest soil erosion values, especially in RCP2.6 and RCP8.5 for 2070 with overall values of 4.25 t ha−1 y−1 and 4.1 t ha−1 y−1, respectively. They were followed by agriculture fields with 1.31 t ha−1 y−1 and 1.33 t ha−1 y−1. The lowest results were located in the residential areas with 0.61 t ha−1 y−1 and 0.63 t ha−1 y−1 in RCP2.6 and RCP8.5 for 2070, respectively. In contrast, RCP4.5 showed that the total soil erosion could experience a decrease in rangelands by − 0.24 t ha−1 y−1 (2050), and − 0.18 t ha−1 y−1 (2070) or a slight increase in the other land uses. We conclude that this study provides new insights for policymakers and stakeholders to develop appropriate strategies to achieve sustainable land resources planning in semi-arid areas that could be affected by future and unforeseen climate change scenarios.Fatemeh HateffardSafwan MohammedKaram AlsafadiGlory O. EnaruvbeAhmad HeidariHazem Ghassan AbdoJesús Rodrigo-CominoNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-17 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Fatemeh Hateffard
Safwan Mohammed
Karam Alsafadi
Glory O. Enaruvbe
Ahmad Heidari
Hazem Ghassan Abdo
Jesús Rodrigo-Comino
CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
description Abstract Soil erosion (SE) and climate change are closely related to environmental challenges that influence human wellbeing. However, the potential impacts of both processes in semi-arid areas are difficult to be predicted because of atmospheric variations and non-sustainable land use management. Thus, models can be employed to estimate the potential effects of different climatic scenarios on environmental and human interactions. In this research, we present a novel study where changes in soil erosion by water in the central part of Iran under current and future climate scenarios are analyzed using the Climate Model Intercomparison Project-5 (CMIP5) under three Representative Concentration Pathway-RCP 2.6, 4.5 and 8.5 scenarios. Results showed that the estimated annual rate of SE in the study area in 2005, 2010, 2015 and 2019 averaged approximately 12.8 t ha−1 y−1. The rangeland areas registered the highest soil erosion values, especially in RCP2.6 and RCP8.5 for 2070 with overall values of 4.25 t ha−1 y−1 and 4.1 t ha−1 y−1, respectively. They were followed by agriculture fields with 1.31 t ha−1 y−1 and 1.33 t ha−1 y−1. The lowest results were located in the residential areas with 0.61 t ha−1 y−1 and 0.63 t ha−1 y−1 in RCP2.6 and RCP8.5 for 2070, respectively. In contrast, RCP4.5 showed that the total soil erosion could experience a decrease in rangelands by − 0.24 t ha−1 y−1 (2050), and − 0.18 t ha−1 y−1 (2070) or a slight increase in the other land uses. We conclude that this study provides new insights for policymakers and stakeholders to develop appropriate strategies to achieve sustainable land resources planning in semi-arid areas that could be affected by future and unforeseen climate change scenarios.
format article
author Fatemeh Hateffard
Safwan Mohammed
Karam Alsafadi
Glory O. Enaruvbe
Ahmad Heidari
Hazem Ghassan Abdo
Jesús Rodrigo-Comino
author_facet Fatemeh Hateffard
Safwan Mohammed
Karam Alsafadi
Glory O. Enaruvbe
Ahmad Heidari
Hazem Ghassan Abdo
Jesús Rodrigo-Comino
author_sort Fatemeh Hateffard
title CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
title_short CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
title_full CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
title_fullStr CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
title_full_unstemmed CMIP5 climate projections and RUSLE-based soil erosion assessment in the central part of Iran
title_sort cmip5 climate projections and rusle-based soil erosion assessment in the central part of iran
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/bd1bbdf84f944ecc9f652ec00bbbd71a
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