2020
DOI: 10.1016/j.jafrearsci.2020.103871
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A new simple approach to assess sediment yield at a large scale with high landscape diversity: an example of Morocco

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Cited by 7 publications
(6 citation statements)
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“…Meseta domains are formed by a Paleozoic basement of Cambrian to Carboniferous age and consist mainly of sedimentary terrain with intense bimodal volcanic activity in the Visean; it is generally characterized by low to moderate relief, well-developed soils and a semi-arid to mediterranean climate. The domain of Anti-Atlas and Sahara (where is the lowest point of the country, at 55 meters below sea level) which is formed by a Proterozoic basement and characterized by a desert climate (P < 100 mm), a vegetation cover dominated essentially by bare areas and sparse desert steppes, and very poor soils (Gourfi et al, 2020;Verner et al, 2018;Michard et al, 2008). Namely, in a semi-arid environment in northwest Morocco that is affected by the formation of severe gullies, where the effects of extreme rainfall are clearly demonstrated (Shrestha and Jetten, 2018).…”
Section: Study Areamentioning
confidence: 99%
“…Meseta domains are formed by a Paleozoic basement of Cambrian to Carboniferous age and consist mainly of sedimentary terrain with intense bimodal volcanic activity in the Visean; it is generally characterized by low to moderate relief, well-developed soils and a semi-arid to mediterranean climate. The domain of Anti-Atlas and Sahara (where is the lowest point of the country, at 55 meters below sea level) which is formed by a Proterozoic basement and characterized by a desert climate (P < 100 mm), a vegetation cover dominated essentially by bare areas and sparse desert steppes, and very poor soils (Gourfi et al, 2020;Verner et al, 2018;Michard et al, 2008). Namely, in a semi-arid environment in northwest Morocco that is affected by the formation of severe gullies, where the effects of extreme rainfall are clearly demonstrated (Shrestha and Jetten, 2018).…”
Section: Study Areamentioning
confidence: 99%
“…Numerous studies have used the accumulated sediments in reservoirs and lakes to estimate sediment yield (SY), while its comparison with estimated gross soil erosion rates also provides a better understanding of sediment transport and sediment sinks (Grauso et al, 2008;Zhang et al, 2006Zhang et al, , 2009Zhao et al, 2017). Reservoir sedimentation can also be used for calibration and validation of erosion models (de Vente et al, 2008;Gourfi et al, 2020;Kotti et al, 2018;Quiñonero-Rubio et al, 2016;Zhao et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…Our current understanding of erosion rates in semi‐arid to arid settings owing to overland flow and gully erosion is still limited, despite significant advances in recent years (Armoza‐Zvuloni et al, 2022; Diani et al, 2023; Mor‐Mussery & Laronne, 2020). One of the main challenges in evaluating erosion rates in these regions is the variability of the landscape and the complexity of the erosion processes (de la Torre‐Robles et al, 2023; García‐Ruiz et al, 2013; Gourfi et al, 2020). In arid and semi‐arid areas, rainfall is often infrequent and intense, leading to flash floods that can cause rapid erosion and transport of sediment (Farhan & Ayed, 2017).…”
Section: Introductionmentioning
confidence: 99%
“…Vegetation lowers ground surface temperatures by providing shade [12,13]. Trees and vegetation decrease ambient air temperature through the process of evapotranspiration, where they release water vapour into the atmosphere [14,15]. In fact, areas with very high temperatures are characterised either by an absence of vegetation or by predominantly artificial impermeable surfaces, such as roads, buildings, pavement, etc.…”
Section: Introductionmentioning
confidence: 99%