Abstract
The climatic evolution of the Bani river watershed, the main tributary to the upper Niger River, is approached through the spatiotemporal variability of rainfall grids over the 1950–2006 period. The analyses are conducted, and their results compared, using four different methods of spatial interpolation of rainfall fields: the spline, kriging, weighted inverse distance, and nearest neighbor methods. The largest changes are observed for all of these grids, but differences—and in some cases divergent results—appear in the details. The analysis shows a substantial decline in rainfall, particularly marked in the center of the basin, during the 1970–2000 period with respect to the 1950–1969 period, and a slight upturn in the northern part, mainly since the beginning of the 1990s. The rainfall deficit can be attributed to a combination of factors: an earlier and drier end of the rainy season, less precipitation in the middle of the rainy season, more dry days and lower amounts of precipitation on rainy days. Two drought indices—the Effective Drought Index and Standardized Precipitation Index—revealed that the maximum duration of drought events increased most in the central part of the basin. Lastly, to supplement this comparison of methods of spatial interpolation of rainfall fields, the sensitivity of a hydrological model (GR2M) to rainfall data was tested. Given the distribution and density of rain gauge stations available in the Bani watershed, the kriging method is found to yield the best hydrological modeling performance.
Similar content being viewed by others
References
Ali A, Lebel T, Amani A (2008) Signification et usage de l'indice pluviométrique au Sahel. Sécheresse 19:227–235
Bamba F, Diabaté M, Mahé G, Diarra M (1997) Bilans hydrologiques pour des affluents majeurs du fleuve Niger: le Bani, le Sankarani, le Tinkisso et le Milo. Doc Tech Hydrol l'UNESCO 16:65–82
Billen G, Garnier J, Hanset P (1994) Modelling phytoplankton development in whole drainage network: the RIVERSTRAHLER model applied to the Seine river system. Hydrobiologia 289:119–137
Boyer JF, Dieulin C, Rouché N, Crès A, Servat E, Paturel JE, Mahé G (2006) SIEREM: an environmental information system for water resources. In: Water resource variability: processes, analyses and impacts. IAHS, 308, pp 19-25.
Briggs IC (1974) Machine contouring using minimum curvature. Geophysics 39:39–48
Byun HR, Wilhite DA (1999) Objective quantification of drought severity and duration. J Clim 12:2747–2756
Conway D (1997) A water balance model of the Upper Blue Nile in Ethiopia. Hydrol Sci J 42:841–859
Conway D, Mahe G (2009) Riverflow modelling in two large river basins: the Parana (subtropical) and the Niger (tropical). Hydrol Process 23:3186–3192
Cressie NA (1990) The origins of kriging. Math Geol 22:239–252
Davis JC (1986) Statistics and data analysis in geology. Wiley, New-York, 656p
Folland CK, Palmer TN, Parker DE (1986) Sahel rainfall and worldwide sea temperature. Nature 320:602–607
Franke R (1982) Scattered data interpolation: test of some methods. Math Comput 33:181–200
Janicot S, Fontaine B (1993) L'évolution des idées sur la variabilité interannuelle récente des précipitations en Afrique de l'Ouest. Météorol 8:28–53
Kasei R, Diekkrüger B, Leemhuis C (2009) Drought frequency in the Volta Basin of West Africa. Sustain Sci 5:89–97
Laux P, Wagne S, Wagner A, Jacobeit J, Bardossy A, Kunstmann H (2009) Modelling daily precipitation features in the Volta Basin of West Africa. Int J Climatol 29:937–954
Le Barbé L, Lebel T, Tapsoba D (2002) Rainfall variability in West Africa during the years 1950–90. J Clim 15:187–202
Lloyd-Hughes B, Saunders MA (2002) A drought climatology for Europe. Int J Climatol 22:1571–1592
Louvet S, Fontaine B, Roucou P (2003) Active phases and pauses during the installation of the West African monsoon through 5-day CMAP rainfall data (1979–2001). Geophys Res Lett 30:2271–2275
Mahé G (2009) Surface/groundwater relationships in two great river basins in West Africa, Niger and Volta. Hydrol Sci J 54:704–712
Mahé G, Olivry JC (1999) Assessment of freshwater yields to the ocean along the intertropical Atlantic coast of Africa. C R Acad Sci 328:621–626
Mahé G, Paturel JE (2009) 1896–2006 Sahelian annual rainfall variability and runoff increase of Sahelian Rivers. Compt Rendus Geosci 341:538–546
Mahé G, Olivry JC, Dessouassi R, Orange D, Bamba F, Servat E (2000) Relations eaux de surface-eaux souterraines d’une rivière tropicale au Mali. C R Acad Sci 330:689–692
Mahé G, L’Hote Y, Olivry JC, Wotling G (2001) Trends and discontinuities in regional rainfall of West and Central Africa: 1951–1989. Hydrol Sci 46:211–226
Mahe G, Girard S, New M, Paturel JE, Cres A, Dezetter A, Dieulin C, Boyer JF, Rouche N, Servat E (2008) Comparing available rainfall gridded datasets for West Africa and the impact on rainfall-runoff modelling results, the case of Burkina-Faso. Water SA 34:529–536
Makhlouf Z, Michel C (1994) A two-parameter monthly water balance model for French watersheds. J Hydrol 162:299–318
Mc Kee TB, Doesken NJ, Kleist J (1993) The relationship of drought frequency and duration to time scale. Rep Eighth Conf Appl Climatol 6
Nash JE, Sutcliffe JV (1970) River flow forecasting through conceptual models, a discussion of principles. J Hydrol 10:282–290
Nicholson S, Palao I (1993) A re-evaluation of rainfall variability in the Sahel. Part 1. Characteristics of rainfall fluctuations. Int J Climatol 13:371–389
Pettitt AN (1979) A non-parametric approach to the change-point problem. Appl Stat 28:126–135
Redelsperger JL, Thorncroft CD, Diedhiou A, Lebel T, Parker DJ, Polcher J (2006) African monsoon multidisciplinary analysis—an international research project and field campaign. Bull Am Meteorol Soc 87:1739–1746
Rouault M, Richard Y (2003) Intensity and spatial extension of drought in South Africa at different time scales. Water SA 29:489–500
Roudier P, Mahé G (2009) Study of water stress and droughts with indicators using daily data on the Bani river (Niger basin, Mali). Int J Climatol 30(11):1689–1705
Ruelland D, Ardoin-Bardin S, Billen G, Servat E (2008) Sensitivity of a lumped and semi-distributed hydrological model to several modes of rainfall interpolation on a large basin in West Africa. J Hydrol 361:96–117
Servat E, Paturel JE, Kouame B, Travaglio M, Ouedraogo M, Boyer JF, Lubes-Niel H, Fritsch JM, Masson JM, Marieu B (1998) Identification, characterization and consequences of an hydrological variability in western and central Africa. Water resources variability in Africa during the XXth century. Int Conf 252:323–337
Sultan B, Janicot S (2003) The West African monsoon dynamics. Part II: The "Preonset" and the "Onset" of the summer Monsoon. J Clim 16:3407–3427
Vörösmarty CJ, Douglas EM, Green PA, Revenga C (2005) Geospatial indicators of emerging water stress: an application to Africa. AMBIO 34:230–237
Acknowledgments
The research for this paper was conducted as part of the RESSAC research project, which received funding from the French National Research Agency (ANR) under a call for research projects entitled “Vulnerability: Environments and Climate” in 2006. We also thank the field personnel and data management organizations who made their data available to us. Without them, no scientific research would be possible.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Louvet, S., Paturel, J.E., Mahé, G. et al. Comparison of the spatiotemporal variability of rainfall from four different interpolation methods and impact on the result of GR2M hydrological modeling—case of Bani River in Mali, West Africa. Theor Appl Climatol 123, 303–319 (2016). https://doi.org/10.1007/s00704-014-1357-y
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00704-014-1357-y