Abstract
Heavy rainfall episodes are relatively common in the conurbation of Barcelona and neighbouring cities (NE Spain), usually due to storms generated by convective phenomena in summer and eastern and south-eastern advections in autumn. Prevention of local flood episodes and right design of urban drainage have to take into account the rainfall intensity spread instead of a simple evaluation of daily rainfall amounts. The database comes from 5-min rain amounts recorded by tipping buckets in the Barcelona urban network along the years 1994–2009. From these data, extreme 5-min rain amounts are selected applying the peaks-over-threshold method for thresholds derived from both 95% percentile and the mean excess plot. The return period curves are derived from their statistical distribution for every gauge, describing with detail expected extreme 5-min rain amounts across the urban network. These curves are compared with those derived from annual extreme time series. In this way, areas in Barcelona submitted to different levels of flood risk from the point of view of rainfall intensity are detected. Additionally, global time trends on extreme 5-min rain amounts are quantified for the whole network and found as not statistically significant.
Similar content being viewed by others
References
Acero FJ, García JA, Gallego MC (2011) Peaks-over-threshold study of trends in extreme rainfall over the Iberian Peninsula. J Clim 24:1089–1105
Alhakim A, Hooper W (2008) A non-parametric test for several independent samples. Journal of Nonparametric Statistics 20(3):253–261. https://doi.org/10.1080/10485250801976741
Anagnostopoulou C, Tolika K (2012) Extreme precipitation in Europe: statistical threshold selection based on climatological criteria. Theor Appl Climatol 107:479–489
Beguería-Portugués S (2005) Uncertainties in partial duration series modelling of extremes related to the choice of the threshold value. J Hydrol 303:215–230
Beguería S, Vicente-Serrano SM, López-Moreno JI, García-Ruíz JM (2009) Annual and seasonal mapping of peak intensity, magnitude and duration of extreme precipitation events across a climatic gradient, North-East Spain. Int J Climatol 29:1759–1779
Beguería S, Angulo-Martínez M, Vicente-Serrano SM, López-Moreno JI, El-Kenawi A (2011) Assessing trends in extreme precipitation events intensity and magnitude using non-stationary peaks-over-threshold analysis: a case study in North-East Spain from 1930 to 2006. Int J Climatol 31:2102–2114
Benjamin JR, Cornell CA (1970) Probability, statistics and decision for civil engineers. McGraw-Hill Inc., New York NY
Burgueño A, Serra C, Lana X (2004) Monthly and annual statistical distributions of the daily rainfall at the Fabra Observatory (Barcelona, NE Spain) for the years 1917–1999. Theor Appl Climatol 77:57–75
Casas MC, Codina B, Redaño A, Lorente J (2004) A methodology to classify extreme rainfall events in the western Mediterranean area. Theor Appl Climatol 77:139–150. https://doi.org/10.1007/s00704-003-0003-x
Casas MC, Rodríguez R, Redaño A (2010) Analysis of extreme rainfall in Barcelona using a microscale rain gauge network. Meteorol Appl 17:117–123. https://doi.org/10.1002/met.166 http://hdl.handle.net/2117/6733
Chen YR, Chu P-S (2014) Trends in precipitation extremes and return levels in the Hawaiian Islands and their changing climate. Int J Climatol 34:3913–3925
Claps P, Laio F (2003) Can continuous streamflow data support flood frequency analysis? An alternative to the partial duration series approach. Water Resour Res 39:1216
Coles S (2001) An introduction to statistical modeling of extreme values. Springer Science and Business Media, 208 pp
Ferguson TS, Genest C, Hallin M (2000) Kendall’s tau for serial dependence. Canadian Journal of Statistics 28:587–604
Hosking JRM, Wallis JR, Wood EF (1985) Estimation of the generalised extreme value distributions by the method of probability-weighted moments. Techtonometrics 27:251–261
Hosking JRM, Wallis JR (1997) Regional frequency analysis. Cambridge University Press, Cambridge, 224 pp
Kendall MG, Stuart A (1967) The advanced theory of statistics, vol 2. Inference and relationship, 2nd edn. Griffin, London
Kysely J, Picek J, Veranová R (2010) Estimating extremes in climate change simulations using the peaks-over-threshold method with non-stationary threshold. Glob Planet Chang 72:55–68
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
Lana X, Martínez MD, Serra C, Burgueño A (2005) Periodicities and irregularities of indices describing the daily pluviometric regime of the Fabra Observatory (NE Spain) for the years 1917–1999. Theor Appl Climatol 82:183–198
Lana X, Serra C, Casas-Castillo MC, Rodríguez-Solà R, Redaño A, Burgueño A (2017) Rainfall intensity patterns derived for the urban network of Barcelona (NE Spain). Theor Appl Climatol. https://doi.org/10.1007/s00704-017-2193-7
Lorente J, Redaño A (1990) Rainfall rate distribution in a local scale: the case of Barcelona City. Theor Appl Climatol 41:23–32
Mitchell JM, Dzerdzeevskii B, Flohn H, Hofmeyr WL, Lamb HH, Rao KN, Wall’en CC. 1966. Climatic change. Technical Note, No. 79. World Meteorological Organization: Geneva, Switzerland, 99
Press WH, Teukolsky SA, Vetterling WT, Flannery BP (1992) Numerical recipes in C. The art of scientific computing. Cambridge University Press, Cambridge, 994 pp
Rodríguez, R., Navarro, X., Casas, M.C., Redaño, A. (2013a). Rainfall spatial organization and areal reduction factors in the metropolitan area of Barcelona (Spain). Theor Appl Climatol, 114, 1–8. DOI: https://doi.org/10.1007/s00704-012-0818-4. http://hdl.handle.net/2117/17169
Rodríguez, R., Casas, M.C., Redaño, A. (2013b). Multifractal analysis of the rainfall time distribution on the metropolitan area of Barcelona (Spain). Meteorol Atmospheric Physics, 121(3–4): 181–187, doi https://doi.org/10.1007/s00703-013-0256-6. http://hdl.handle.net/2117/19110
Rodríguez-Solà R, Casas-Castillo MC, Navarro X, Redaño A (2016) A study of the scaling properties of rainfall in Spain and its appropriateness to generate intensity-duration-frequency curves from daily records. Int J Climatol 37:770–780. https://doi.org/10.1002/joc.4738. http://hdl.handle.net/2117/87312
Sneyers R (1990) On the statistical analysis of series of observations. In: Technical note 415. WMO, Geneva
Vicente-Serrano SM, Beguería-Portugués S (2003) Estimating extreme dry-spell risk in the middle Ebro valley (NE Spain): a comparative analysis of partial duration series with general Pareto distribution and annual maxima series with a Gumbel distribution. Int J Climatol 23:1103–1118
Villarini G, Smith JA, Ntelekos AA, Schwartz U (2011) Annual maximum and peaks-over-threshold analyses of daily rainfall accumulations for Austria. J Geophys Res 116:D05103
Author information
Authors and Affiliations
Corresponding author
Appendix. Kendall-τ test of independence
Appendix. Kendall-τ test of independence
If a set of {zi}, i = 1,…,n, peaks are selected from a time series and their associated ranks, {Ri} are determined, the Kendall-τ test can be applied to verify the independence of the series, usually with a probability exceeding 95%. After obtaining the set of rank pairs {(R1, R2), (R2, R3), ….., (Rn−1, Rn)}, the number of discordances nd or, in other words, the number of pairs (Ri, Ri+1) and (Rj, Rj+1) accomplishing either Ri < Rj and Ri+1 > Rj+1 or Ri > Rj and Ri+1 < Rj+1, with i = 1,…,n−1, j = 1,…,n−1 and i ≠ j leads to the empiric Kendall-τ statistic
The null hypothesis of independent {zi} peaks approaches τ to a normal random variable, provided that the number of samples n exceeds 10. The expected value of τ will be
and its variance
If τemp, given by Eq. (9), does not exceed
the one-sided 95% test permits accepting the null hypothesis of {zi} independence with 95% confidence.
Rights and permissions
About this article
Cite this article
Lana, X., Casas-Castillo, M.C., Serra, C. et al. Return period curves for extreme 5-min rainfall amounts at the Barcelona urban network. Theor Appl Climatol 135, 1243–1257 (2019). https://doi.org/10.1007/s00704-018-2434-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00704-018-2434-4