Abstract
Rainfall intensity, duration, frequency and magnitude influence both runoff generation and sediment yield. In this study, 176 rainfall events over a five-year period were classified into four regimes based on rainfall depth, duration and 30-minute maximum intensity, using hierarchical cluster analysis in the semiarid region of Brazil. Rainfall Regimes were grouped from higher to lower rainfall depth, longer to shorter duration, and higher to lower I30. Rainfall regime impact on surface runoff and sediment yield was studied in three watersheds under different land use - native tropical dry forest, thinned tropical dry forest, and slash and burn followed by grass cultivation. Thinning of native dry tropical forest reduced surface runoff and sediment yield due to the protective effect of the well-developed herbaceous layer. Runoff generation in the three watersheds showed strong dependence on antecedent soil moisture and the type of rain. Rainfall depth was the major factor for highest sediment yields.
Similar content being viewed by others
References
Arnau-Rosalén E, Calvo-Cases A, Boix-Fayos C, Lavee H, Sarah P (2008) Analysis of soil surface component patterns affecting runoff generation. An example of methods applied to Mediterranean hillslopes in Alicante (Spain). Geomorphology 101(4):595–606. doi:10.1016/j.geomorph.2008.03.001
Bracken LJ, Croke J (2007) The concept of hydrological connectivity and its contribution to understanding runoff-dominated geomorphic systems. Hydrol Process 21(13):1749–1763. doi:10.1002/hyp.6313
Dinka TM, Morgan CLS, McInnes KJ, Kishné ASZ, Harmel RD (2013) Shrink–swell behavior of soil across a vertisol catena. J Hydrol 476:352–359. doi:10.1016/j.jhydrol.2012.11.002
Fang N, Shi Z, Li L, Guo Z, Liu Q, Ai L (2012) The effects of rainfall regimes and land use changes on runoff and soil loss in a small mountainous watershed. Catena 99:1–8. doi:10.1016/j.catena.2012.07.004
Ferreira AG, Mello NGS (2005) Principais sistemas atmosféricos atuantes sobre a região Nordeste do Brasil e a influência dos oceanos Pacífico e Atlântico no clima da região. Rev Bras Clim 1(1):15–28
Fryirs KA, Brierley GJ, Preton NJ, Kasai M (2007) Buffers, barriers and blankets: the (dis) connectivity of catchment-scale sediment cascades. Catena 70:49–68. doi:10.1016/j.catena.2006.07.007
Guerreiro MJS, Andrade EM, Abreu I, Lajinha T (2013) Long-term variation of rainfall indices in Ceará State Northeast Brazil. Int J Climatol. doi:10.1002/joc.3645
Harmel RD, Richardson CW, King KW, Allen PM (2006) Runoff and soil loss relationships for the Texas Blackland Prairies ecoregion. J Hydrol 331:471–483. doi:10.1016/j.jhydrol.2006.05.033
James AL, Roulet NT (2009) Antecedent moisture conditions and catchment morphology as controls on spatial patterns of flow generation in small forest catchments. J Hydrol 377(3–4):351–366. doi:10.1016/j.jhydrol.2009.08.039
Kishné ASZ, Morgan CLS, Ge Y, Miller WL (2010) Antecedent soil moisture affecting surface cracking of a vertisol infield conditions. Geoderma 157:109–117. doi:10.1016/j.geoderma.2010.03.020
Krasilnikov P, Ibáñez JJ, Arnold R, Shoba S (2009) A handbook of soil terminology, correlation and classification. Routledge, UK, p 448
Kumar S, Mishra A (2015) Critical erosion area identification based on hydrological response unit level for effective sedimentation control in a river basin. Water Resour Manag 29(6):1749–1765. doi:10.1007/s11269-014-0909-3
Mallinis G, Gitas IZ, Tasionas G, Maris F (2016) Multitemporal monitoring of land degradation risk Due to soil loss in a fire-prone Mediterranean landscape using multi-decadal Landsat imagery. Water Resour Manag 30(3):1255–1269. doi:10.1007/s11269-016-1224-y
Medeiros PHA, de ARAÚJO JC (2014) Temporal variability of rainfall in a semiarid environment in Brazil and its effect on sediment transport processes. J Soils Sediments 14:1216–1223. doi:10.1007/s11368-013-0809-9
Medeiros PHA, Güntner A, Francke T, Mamede GL, de Araújo JC (2010) Modelling spatio-temporal patterns of sediment yield and connectivity in a semi-arid catchment with the WASA-SED model. Hydrol Sci J 55:636–648. doi:10.1080/02626661003780409
Molina-Navarro E, Martínez-Pérez S, Sastre-Merlín A, Bienes-Allas R (2014) Catchment erosion and sediment delivery in a Limno-reservoir basin using a simple methodology. Water Resour Manag 28(8):2129–2143. doi:10.1007/s11269-014-0601-7
Morin E, Goodrich DC, Maddox RA (2006) Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response. Adv Water Resour 29(6):843–860. doi:10.1016/j.advwatres.2005.07.014
Nóbrega RS, Santiago GACF (2014) Tendência de temperatura na superfície do mar nos oceanos atlântico e pacífico e variabilidade de precipitação em Pernambuco. Mercator 13(1):107–118. doi:10.4215/RM2014.1301.0008
Peng T, Wang S (2012) Effects of land use, land cover and rainfall regimes on the surface runoff and soil loss on karst slopes in southwest China. Catena 90:53–62. doi:10.1016/j.catena.2011.11.001
Poesen J, Nachtergaele J, Verstraeten G, Valentin C (2003) Gully erosion and environmental change: importance and research needs. Catena 50:91–133. doi:10.1016/S0341-8162(02)00143-1
Rodrigues JO, Andrade EM, Palácio HAQ, Mendonça LAR, Santos JCN (2013) Sediment loss in semiarid small watershed due to the land use. Rev Ciênc Agron 44(3):488–498. doi:10.1590/S1806-66902013000300010
Santos JCN, Andrade EM, Guerreiro MJS, Medeiros PHA, Palácio HAQ, Araújo Neto JR (2016) Effect of dry spells and soil cracking on runoff generation in a semiarid micro watershed under land use change. J Hydrol 541(Part B):1057–1066. doi:10.1016/j.jhydrol.2016.08.016
Sen S, Srivastava P, Jacob DH (2010) Spatial–temporal variability and hydrologic connectivity of runoff generation areas in a North Alabama pasture-implications for phosphorus transport. Hydrol Process 24(3):342–356. doi:10.1002/hyp.7502
Smith MW, Bracken LJ, Cox NJ (2010) Toward a dynamic representation of hydrological connectivity at the hillslope scale in semiarid areas. Water Resour Res 46, W12540. doi:10.1029/2009WR008496
Ulke A, Tayfur G, Ozkul S (2016) Investigating a suitable empirical model and performing regional analysis for the suspended sediment load prediction in major rivers of the Aegean region. Turkey Water Resour Manag. doi:10.1007/s11269-016-1357-z
Wei W, Chen L, Fu B, Huang B, Wu D, Gui L (2007) The effect of land uses and rainfall regimes on runoff and soil erosion in the semi-arid loess hilly area, China. J Hydrol 335(3–4):247–258. doi:10.1016/j.jhydrol.2006.11.016
Wei W, Jia F, Yang L, Chen L, Zhang H (2014) Effects of surficial condition and rainfall intensity on runoff in a loess hilly area, China. J Hydrol 513:115–126. doi:10.1016/j.jhydrol.2014.03.022
Wester T, Wasklewicz T, Staley D (2014) Functional and structural connectivity within a recently burned drainage basin. Geomorphology 206:362–373. doi:10.1016/j.geomorph.2013.10.011
Yang T, Wang Q, Su L, Wu L, Zhao G, Liu Y, Zhang P (2016) An approximately semi-analytical model for describing surface runoff of rainwater over sloped land. Water Resour Manag. doi:10.1007/s11269-016-1400-0
Zhang X, Yu GQ, Li ZB, Li P (2014a) Experimental study on slope runoff, erosion and sediment under different vegetation types. Water Resour Manag 28(9):2415–2433. doi:10.1007/s11269-014-0603-5
Zhang ZB, Zhou H, Zhao QG, Lin H, Peng X (2014b) Characteristics of cracks in two paddy soils and their impacts on preferential flow. Geoderma 228–229:114–121. doi:10.1016/j.geoderma.2013.07.026
Acknowledgments
The authors would like to acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) and the Coordination for the Improvement of Higher Education Personnel (CAPES) for the financial support to this research, and the valuable contribution of the anonymous reviewers.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
dos Santos, J.C.N., de Andrade, E.M., Medeiros, P.H.A. et al. Effect of Rainfall Characteristics on Runoff and Water Erosion for Different Land Uses in a Tropical Semiarid Region. Water Resour Manage 31, 173–185 (2017). https://doi.org/10.1007/s11269-016-1517-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11269-016-1517-1