Abstract
Dry spell and drought are hydrological phenomena with serious socioeconomic effects and, despite recent efforts, substantial scientific and statistical comprehension are still lacking—especially when considering their extreme events. Such events are usually modeled using the generalized extreme value (GEV) distribution, whose prediction performance, at least under a Bayesian approach, remain poorly understood when fitted to a discrete series (the simplest way to record dry spell occurrence and duration). Thus, in this study, we aim at evaluating point and interval prediction performances of the GEV distribution when fitted to dry spell data, using computer simulations of different realistic scenarios (variations in the number of days per dry spells, number of dry spells per year, sample sizes, and available prior information). While sample size increase produced generally expected results over point performance (i.e., stronger bias in small samples), counterintuitive patterns arose when we evaluated the accuracy of prediction credible intervals. We also found a positive correlation between prediction bias and the GEV shape parameter estimate, a fact we believe to be related to the discrete nature of the data. Furthermore, we noticed the best interval performances occurred in increasing levels of information rendered by prior distributions. Finally, we consider all these results to be general enough to apply to different extreme discrete phenomena, since we found no effect of neither the duration nor the frequency of dry spells. Although typical issues in discrete data (e.g., overdispersion) and time series data (e.g., trend) should be considered in future investigations, one must be aware that whenever attempting to fit dry spell duration series to the GEV distribution in the absence of substantial prior information will frequently lead to underestimated predictions—the worst kind for dry spell strategic management—which may further compromise scientists, practitioners, and their community responsibilities.
Similar content being viewed by others
References
Agarwal A, Babel MS, Maskey S (2014) Analysis of future precipitation in the Koshi river basin, Nepal. J Hydrol 513:422–434. https://doi.org/10.1016/j.jhydrol.2014.03.047
Assis JMO (2012) Análise de tendências de mudanças climáticas no semiárido de Pernambuco 166
Beijo LA, Vivanco MJF, Muniz JA (2009) Bayesian analysis for estimating the return period of maximum precipitation at Jaboticabal São Paulo state, Brazil. Ciência e Agrotecnologiancia e Agrotecnologia 33:261–270
Bloomfield JP, Allen DJ, Griffiths KJ (2009) Examining geological controls on baseflow index (BFI) using regression analysis: an illustration from the Thames Basin, UK. J Hydrol 373:164–176
Bond NR, Lake PS, Arthington AH (2008) The impacts of drought on freshwater ecosystems: an Australian perspective. Hydrobiologia 600:1–14. https://doi.org/10.1007/s10750-008-9326-z
Bouagila B, Sushama L (2013) On the current and future dry spell characteristics over Africa. Atmosphere (Basel) 4:272–298
Cancelliere A, Salas JD (2010) Drought probabilities and return period for annual streamflows series. J Hydrol 391:77–89
Coles S (2001) An introduction to statistical modeling of extreme values. Springer-Verlag, London
Coles S, Pericchi L (2003) Anticipating catastrophes through extreme value modelling. J R Stat Soc: Ser C: Appl Stat 52:405–416
Coles S, Powell EA (1996) Bayesian methods in extreme value modelling: a review and new developments. Int Stat Rev 64:119–136
Coles S, Tawn J (2005) Bayesian modelling of extreme surges on the UK east coast. Philos Trans R Soc A 363:1387–1406
Collischonn W, Tucci CEM, Clarke RT (2001) Further evidence of changes in the hydrological regime of the River Paraguay: part of a wider phenomenon of climate change? J Hydrol 245:218–238. https://doi.org/10.1016/S0022-1694(01)00348-1
Dubrovsky M, Svoboda MD, Trnka M, Hayes MJ, Wilhite DA, Zalud Z, Hlavinka P (2009) Application of relative drought indices in assessing climate-change impacts on drought conditions in Czechia. Theor Appl Climatol 96:155–171. https://doi.org/10.1007/s00704-008-0020-x
Farokhnia A, Morid S, Byun HR (2011) Application of global SST and SLP data for drought forecasting on Tehran plain using data mining and ANFIS techniques. Theor Appl Climatol 104:71–81. https://doi.org/10.1007/s00704-010-0317-4
Fisher RA, Tippett LHC (1928) Limiting forms of the frequency distribution of the largest or smallest member of a sample. Math Proc Camb Philos Soc 24:180–190
Genest C, Favre AC (2007) Everything you always wanted to know about copula modeling but were afraid to ask. J Hydrol Eng 12:347–368
Geweke J (1992) Evaluating the accuracy of sampling-based approaches to calculating posterior moments. In: Bernardo JM, Berger JO, Dawid AP, Smith AFM (eds) Bayesian statistics 4. Clarendon Press, Oxford, p 859
Ghile YB, Schulze RE (2009) Use of an ensemble re-ordering method for disaggregation of seasonal categorical rainfall forecasts into conditioned ensembles of daily rainfall for hydrological forecasting. J Hydrol 371:85–97. https://doi.org/10.1016/j.jhydrol.2009.03.019
Gnedenko B (1943) Sur la distribution limite du terme maximum d’une serie aleatoire. Ann Math 44:423–453
Govindaraju RS, Rao AR (2000) Artificial neural networks in hydrology. Kluwer Academic Publishers, Amsterdam
Heidelberger P, Welch PD (1983) Simulation run length control in the presence of an initial transient. Oper Res 31:1109–1144. https://doi.org/10.1287/opre.31.6.1109
IBGE (2010) Brazilian socio-economic database. In: Munic. Soc. Indic. https://goo.gl/kS64D6. Accessed 10 Sep 2017
IBGE (2013) Brazilian socio-economic database. In: Vectorial SHP files Polit. Div. Brazil (in Port. https://goo.gl/JDuRiA. Accessed 17 Aug 2018
Jury MR (2018) Uganda rainfall variability and prediction. Theor Appl Climatol 132:905–919. https://doi.org/10.1007/s00704-017-2135-4
Kebede A, Diekkrüger B, Edossa DC (2017) Dry spell, onset and cessation of the wet season rainfall in the Upper Baro-Akobo Basin, Ethiopia. Theor Appl Climatol 129:849–858. https://doi.org/10.1007/s00704-016-1813-y
Kumagai T, Saitoh TM, Sato Y et al (2004) Transpiration, canopy conductance and the decoupling coefficient of a lowland mixed dipterocarp forest in Sarawak, Borneo: dry spell effects. J Hydrol 287:237–251. https://doi.org/10.1016/j.jhydrol.2003.10.002
Lana X, Burgueño A (1998) Probabilities of repeated long dry episodes based on the Poisson distribution. Theor Appl Climatol 60:111–120
Lana X, Burgueño A, Martínez MD, Serra C (2006) Statistical distributions and sampling strategies for the analysis of extreme dry spells in Catalonia (NE Spain). J Hydrol 324:94–114. https://doi.org/10.1016/j.jhydrol.2005.09.013
Lana X, Martínez MD, Burgueño A, Serra C (2008) Return period maps of dry spells for Catalonia (northeastern Spain) based on the Weibull distribution. Hydrol Sci J 53:48–64. https://doi.org/10.1623/hysj.53.1.48
Ma Q, Zhang J, Sun C, Zhang F, Wu R, Wu L (2017) Drought characteristics and prediction during pasture growing season in Xilingol grassland, northern China. Theor Appl Climatol 133:1–14. https://doi.org/10.1007/s00704-017-2150-5
McKee T, Doesken NJ, Kleist J (1993) The relationship of drought frequency and duration to time scales. 179–184
Meshram SG, Gautam R, Kahya E (2018) Drought analysis in the Tons River Basin, India during 1969-2008. Theor Appl Climatol 132:939–951. https://doi.org/10.1007/s00704-017-2129-2
Mishra AK, Singh VP (2010) A review of drough concepts. J Hydrol 391:202–216
Mishra AK, Singh VP (2011) Drought modeling—a review. J Hydrol 403:157–175
Nadarajah S, Mitov K (2002) Asymptotics of maxima of discrete random variables. Extremes 5:287–294
Paixão Junior BR, Estrela F, Cruz G, Lima M (2010) CodeGeo. In: Brazil shapefiles download (in Port. https://goo.gl/qkfPCp. Accessed 17 Aug 2018
Pasarić Z, Cindrić K (2018) Generalised Pareto distribution: impact of rounding on parameter estimation. Theor Appl Climatol. https://doi.org/10.1007/s00704-018-2494-5
Paudyal P, Bhuju DR, Aryal M (2015) Climate change dry spell impact on agriculture in Salyantar, Dhading, Central Nepal. Nepal J Sci Technol 16:59–68
Pérez-Sánchez J, Senent-Aparicio J (2017) Analysis of meteorological droughts and dry spells in semiarid regions: a comparative analysis of probability distribution functions in the Segura Basin (SE Spain). Theor Appl Climatol 133:1–14. https://doi.org/10.1007/s00704-017-2239-x
Plummer M, Best N, Cowles K, Vines K (2006) CODA: convergence diagnosis and output analysis for MCMC. R News 6:7–11
R Core Team (2017) R: a language and environment for statistical computing
Raftery AE, Lewis SM (1992) One long run with diagnostics: implementation strategies for Markov chain Monte Carlo. Stat Sci 7:493–497. https://doi.org/10.1214/ss/1177011143
Ratan R, Venugopal V (2013) Wet and dry spell characteristics of global tropical rainfall. Water Resour Res 49:3830–3841. https://doi.org/10.1002/wrcr.20275
Roncoli C, Ingram K, Kirshen P (2001) The costs and risks of coping with drought: livelihood impacts and farmers’ responses in Burkina Faso. Clim Res 19:119–132. https://doi.org/10.3354/cr019119
Seleshi Y, Camberlin P (2006) Recent changes in dry spell and extreme rainfall events in Ethiopia. Theor Appl Climatol 83:181–191. https://doi.org/10.1007/s00704-005-0134-3
Sharma TC (1996) Simulation of the Kenyan longest dry and wet spells and the largest rain-sums using a Markov model. J Hydrol 178:55–67. https://doi.org/10.1016/0022-1694(95)02827-7
Singh D, Tsiang M, Rajaratnam B, Diffenbaugh NS (2014) Observed changes in extreme wet and dry spells during the South Asian summer monsoon season. Nat Clim Chang 4:456–461
Smith RL (2003) Statistics of extremes, with applications in environment, insurance and finance. In: Finkenstadt B, Rootzen H (eds) Extreme values in finance, telecommunications, and the environment, 1st edn. Chapman and Hall/CRC, pp 1–78
Stephenson AG (2002) evd: extreme value distributions. R News 2:31–32
Sushama L, Khaliq N, Laprise R (2010) Dry spell characteristics over Canada in a changing climate as simulated by the Canadian RCM. Glob Planet Chang 74:1–14
Thomas T, Nayak PC, Ghosh NC (2014) Irrigation planning for sustainable rain-fed agriculture in the drought-prone Bundelkhand region of Madhya Pradesh, India. J Water Clim Chang 5:408–426. https://doi.org/10.2166/wcc.2014.025
Vicente-Serrano SM, Beguería-Portugués S (2003) Estimating extreme dry-spell risk in the middle Ebro valley (northeastern Spain): a comparative analysis of partial duration series with a general Pareto distribution and annual maxima series with a Gumbel distribution. Int J Climatol 23:1103–1118. https://doi.org/10.1002/joc.934
Wilhite DA, Svoboda MD, Hayes MJ (2007) Understanding the complex impacts of drought: a key to enhancing drought mitigation and preparedness. Water Resour Manag 21:763–774. https://doi.org/10.1007/s11269-006-9076-5
Zin WZW, Jemain AA (2010) Statistical distributions of extreme dry spell in Peninsular Malaysia. Theor Appl Climatol 102:253–264. https://doi.org/10.1007/s00704-010-0254-2
Acknowledgements
The authors thank Mr. Fábio F. Marchetti for his kind and insightful considerations.
Funding
This study was financed in part by the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - Brasil (CAPES) - Finance Code 001.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
ESM 1
(PDF 7337 kb)
Rights and permissions
About this article
Cite this article
Butturi-Gomes, D., Beijo, L.A. & Avelar, F.G. On modeling the maximum duration of dry spells: a simulation study under a Bayesian approach. Theor Appl Climatol 137, 1337–1346 (2019). https://doi.org/10.1007/s00704-018-2684-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00704-018-2684-1