Skip to main content

Advertisement

Log in

Copula-based risk evaluation of droughts across the Pearl River basin, China

  • Original Paper
  • Published:
Theoretical and Applied Climatology Aims and scope Submit manuscript

Abstract

Daily precipitation data for the period of 1960–2005 from 42 precipitation gauging stations in the Pearl River basin were analyzed using the Mann–Kendall trend test and copula functions. The standardized precipitation index method was used to define drought episodes. Primary and secondary return periods were also analyzed to evaluate drought risks in the Pearl River basin as a whole. Results indicated that: (1) in general, the drought tendency was not significant at a 95 % confidence level. However, significant drought trends could be found in November, December, and January and significant wetting trends in June and July. The drought severity and drought durations were not significant at most of the precipitation stations across the Pearl River basin; (2) in terms of drought risk, higher drought risk could be observed in the lower Pearl River basin and lower drought risk in the upper Pearl River basin. Higher risk of droughts of longer durations was always corresponding to the higher risk of droughts with higher drought severity, which poses an increasing challenge for drought management and water resources management. When drought episodes with higher drought severity occurred in the Pearl River basin, the regions covered by higher risk of drought events were larger, which may challenge the water supply in the lower Pearl River basin. As for secondary return periods, results of this study indicated that secondary return periods might provide a more robust evaluation of drought risk. This study should be of merit for water resources management in the Pearl River basin, particularly the lower Pearl River basin, and can also act as a case study for determining regional response to drought changes as a result of global climate changes.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9

Similar content being viewed by others

References

  • Brinbaum ZW (1952) Numerical tabulation of the distribution of Kolmogorov's statistic for finite sample size. J Am Stat Assoc 47(259):425–441

    Article  Google Scholar 

  • Calanca P (2007) Climate change and drought occurrence in the Alpine region: how severe are becoming the extremes. Glob Planet Chang 57:151–160

    Article  Google Scholar 

  • Cancelliere A, Salas DJ (2010) Drought probabilities and return period for annual streamflows series. J Hydrol 391:77–89

    Article  Google Scholar 

  • Fleig AK, Tallaksen LM, Hisdal H, Demuth S (2006) A global evaluation of streamflow drought characteristics. Hydrol Earth Syst Sci 10:535–552

    Article  Google Scholar 

  • Frank J, Masse J (1951) The Kolmogorov–Smirnov Test for goodness of fit. J Am Stat Assoc 46(253):68–78

    Article  Google Scholar 

  • Gemmer M, Fischer T, Jiang T, Su B, Liu L (2011) Trends in precipitation extremes in the Zhujiang River Basin, South China. J Climate 24:750–761

    Article  Google Scholar 

  • Genest C, Rivest L (1993) Statistical inference procedures for bivariate Archimedean copulas. J Am Stat Assoc 88(424):1034–1043

    Article  Google Scholar 

  • Hosking JRM (1990) L-moments: analysis and estimation of distributions using linear combinations of order statistics. J R Stat Soc 52(1):105–124

    Google Scholar 

  • Huard D, Evin G, Anne-Catherine F (2006) Bayesian copula selection. Comput Stat Data Anal 51:809–822

    Article  Google Scholar 

  • Husak JG, Michaelsen J, Funk C (2007) Use of gamma distribution to represent monthly rainfall in Africa for drought monitoring application. Int J Climatol 27:935–944

    Article  Google Scholar 

  • Kao S-C, Govindaraju RS (2010) A copula-based joint deficit index for droughts. J Hydrol 380:121–134

    Article  Google Scholar 

  • Kendall MG (1975) Rank correlation methods. Griffin, London

    Google Scholar 

  • Lei YH, Duan AM (2010) Prolonged dry episodes and drought over China. Int J Climatol. doi:10.1002/joc.2197

  • Lioyd-Hughes B (2010) A spatio-temporal structure-based approach to drought characterisation. Int J Climatol. doi:10.1002/joc.2280

  • Livada I, Assimakopoulos VD (2007) Spatial and temporal analysis of drought in Greece using the Standardized Precipitation Index (SPI). Theor Appl Climatol 89:143–153

    Article  Google Scholar 

  • Mann HB (1945) Nonparametric tests against trend. Econometrica 13:245–259

    Article  Google Scholar 

  • Mckee TB, Doesken NJ, Kleist J (1993) The relationship of drought frequency and duration to time scales. Preprints Eighth Conf on Applied Climatology Anaheim CA. Amer Meteor Soc 179–184

  • Mishra AK, Singh VP (2009) Analysis of drought severity-area-frequency curves using a general circulation model and scenario uncertainty. J Geophys Res 114:D06120. doi:10.1029/2008JD010986

    Article  Google Scholar 

  • Mishra KA, Singh PV (2010) A review of drought concepts. J Hydrol 391:202–216

    Article  Google Scholar 

  • Mitchell JM, Dzerdzeevskii B, Flohn H, Hofmeyr WL, Lamb HH, Rao KN, Wallén CC (1966) Climate change, WMO Technical Note No. 79, World Meteorological Organization, pp 79

  • Nelsen RB (2006) An introduction to copulas. Springer, New York

    Google Scholar 

  • Salvadori G, De Michele C (2004) Frequency analysis via copulas: theoretical aspects and applications to hydrological events. Water Resour Res. doi:10.1029/2004WR003133

  • Shiau JT, Shen HW (2001) Recurrence analysis of hydrologic droughts of differing severity. J Water Res Plan Manag 127(1):30–40

    Article  Google Scholar 

  • von Storch H, Navarra A (eds) (1995) Analysis of climate variability—applications of statistical techniques, pp 334. Springer, New York

    Google Scholar 

  • Wilhite DA (2000) Drought as a natural hazard: concepts and definitions. In: Wilhite DA (ed) Drought: a global assessment. Routledge, London, pp 3–18

    Google Scholar 

  • Wong JS, Zhang Q, Chen YD (2010) Statistical modeling of daily urban water consumption in Hong Kong: trend, changing patterns, and forecast. Water Resour Res 46:W03506. doi:10.1029/2009WR008147

    Article  Google Scholar 

  • Wu H, Hayes JM, Weiss A, Hu Q (2001) An evaluation of the standardized precipitation index, the China-Z index and the statistical Z-score. Int J Climatol 21:745–758

    Google Scholar 

  • Yang T, Shao Q, Hao Z-C, Chen X, Zhang Z, Xu C-Y, Sun L (2010) Regional frequency analysis and spatio-temporal pattern charaterization of rainfall extremes in the Pearl River basin, China. J Hydrol 380:386–405

    Google Scholar 

  • Yevjevich V (1967) An objective approach to definitions and investigation of continental hydrologic droughts. Hydrology Paper 23. Colorado State University, Fort Collins

    Google Scholar 

  • Zhang JQ (2004) Risk assessment of drought disaster in the maize-growing region of Songliao Plain, China. Agric Ecosyst Environ 102:133–153

    Article  Google Scholar 

  • Zhang L, Singh VP (2006) Bivariate flood frequency analysis using the copula method. J Hydrol Eng 11:150–164

    Article  Google Scholar 

  • Zhang L, Singh VP (2007) Bivariate rainfall frequency distributions using Archimedean copulas. J Hydrol 332:93–109

    Article  Google Scholar 

  • Zhang X, Harvey D, Hogg WD, Yuzyk TR (2001) Trends in Canadian streamflow. Water Resour Res 37(4):987–998

    Article  Google Scholar 

  • Zhang Q, Xu C-Y, Zhang Z (2008) Observed changes of drought/wetness episodes in the Pearl River basin, China, using the standardized precipitation index and aridity index. Theor Appl Climatol 98:89–99

    Article  Google Scholar 

  • Zhang Q, Xu C-Y, Gemmer M, Chen YD, Liu C-L (2009a) Changing properties of precipitation concentration in the Pearl River basin, China. Stoch Env Res Risk A 23:377–385

    Article  Google Scholar 

  • Zhang Q, Xu C-Y, Becker S, Zhang ZX, Chen YD, Coulibaly M (2009b) Trends and abrupt changes of precipitation extremes in the Pearl River basin, China. Atmos Sci Lett 10:132–144

    Article  Google Scholar 

  • Zhang Q, Xu C-Y, Zhang Z, Chen YD (2010) Changes of atmospheric water vapor budget in the Pearl River basin and possible implications for hydrological cycle. Theor Appl Climatol 102:185–195

    Article  Google Scholar 

  • Zhang Q, Zhang W, Chen YD, Jiang T (2011) Flood, drought and typhoon disasters during the last half century in the Guangdong Province, China. Nat Hazards 57:267–278

    Article  Google Scholar 

  • Zolina O, Simmer C, Gulev SK, Kollet S (2010) Changing structure of European precipitation: longer wet periods leading to more abundant rainfalls. Geophys Res Lett 37:L06704

    Article  Google Scholar 

Download references

Acknowledgments

This work is financially supported by the Program for New Century Excellent Talents in University (the Fundamental Research Funds for the Central Universities), the National Natural Science Foundation of China (grant no.: 41071020; 50839005), the Project from Guangdong Science and Technology Department (grant no.: 2010B050800001; 2010B050300010), a grant from the Research Grants Council of the Hong Kong Special Administrative Region, China (project no. CUHK405308), and by the Geographical Modeling and Geocomputation Program under the Focused Investment Scheme (1902042) of The Chinese University of Hong Kong. The last but not the least, our cordial gratitude should be extended to the editor, Prof. Dr. Hartmut Grassl and anonymous reviewers for their invaluable comments which greatly helped to improve the quality of this paper.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Qiang Zhang.

Appendix

Appendix

The Copula family is described as the follows.

  1. 1.

    Gumbel–Hougaard (GH) family

    The GH family can be formulated as:

    $$ C\left( {u,v} \right) = \exp \left\{ { - {{\left[ {{{\left( { - \ln u} \right)}^\theta } + {{\left( { - \ln v} \right)}^\theta }} \right]}^{1/\theta }}} \right\},\theta \in \left[ {1,\infty } \right) $$
    (9)

    where u and v are the marginal distribution functions of two hydrological variables; θ is the parameter of the GH family; C is the copula having the function of capturing the essential features of the dependence among random variables. Parameters u, v, and θ in the following equations have the same meaning as those in Eq. (9), so no further explanations are provided thereafter. The copula generator of the GH family (Zhang and Singh 2007) is:

    $$ \phi (t) = {\left( { - \ln t} \right)^\theta } $$
    (10)

    t is the u 1 or v 1, being specific values of u and v in Eq. (9) varying from 0 to 1. The relationship between parameter, θ, and Kendall’s coefficient of correlation, τ, between X and Y is τ = 1 − θ −1. The GH copula performs well in the description of the correlation structure of two variables characterized by a positive correlation.

  2. 2.

    Clayton family

    The Clayton family can be formulated as:

    $$ C\left( {u,v} \right) = {\left( {{u^{ - \theta }} + {v^{ - \theta }} - 1} \right)^{ - 1/\theta }},\theta \in \left( {0,\infty } \right) $$
    (11)

    The copula generator of Clayton family is

    $$ \varphi (t) = \left( {{t^{ - \theta }} - 1} \right)/\theta, \theta \in \left( {0,\infty } \right) $$
    (12)

    The relation between parameter, θ, and Kendall’s coefficient of correlation, τ, between X and Y is:

    $$ \tau = \frac{\theta }{{2 + \theta }},\theta \in \left( {0,\infty } \right) $$
    (13)

    The Clayton family is good for describing two variables with a positive correlation.

  3. 3.

    Frank family

    The Frank family can be formulated as:

    $$ C\left( {u,v} \right) = - \frac{1}{\theta }\ln \left[ {1 + \frac{{\left( {{e^{ - \theta u}} - 1} \right)\left( {{e^{ - \theta v}} - 1} \right)}}{{\left( {{e^{ - \theta }} - 1} \right)}}} \right],\theta \in R $$
    (14)

    The copula generator of the Clayton family is

    $$ \varphi (t) = - \ln \frac{{{e^{ - \theta t}} - 1}}{{{e^{ - \theta }} - 1}},\theta \in R $$
    (15)

    The relation between parameter, θ, and Kendall’s coefficient of correlation, τ, between X and Y is:

    $$ \tau = 1 + \frac{4}{\theta }\left[ {\frac{1}{\theta }\int\limits_0^\theta {\frac{t}{{{e^t} - 1}}dt - 1} } \right],\theta \in R $$
    (16)

    The Frank family performs well for describing two variables with a positive correlation.

  4. 4.

    t copula family

    The t family can be formulated as:

    $$ C_{v,R}^t\left( {u,v} \right) = {\int_{ - \infty }^{t_v^{ - 1}(u)} {\int_{ - \infty }^{t_v^{ - 1}(v)} {\frac{1}{{2\pi {{\left( {1 - {\theta^2}} \right)}^{\frac{1}{2}}}}}\left[ {1 + \frac{{{s^2} - 2\theta st + {t^2}}}{{v\left( {1 - {\theta^2}} \right)}}} \right]} }^{ - \frac{{\left( {v + 2} \right)}}{2}}}dsdt $$
    (17)

    \( t_{v,R}^n \) is the R-dimensional standard t distribution with degree of freedom of v. \( t_v^{ - 1} \) is the inverse function of \( t_{v,R}^n \).

    The relation between parameter, θ, and Kendall’s coefficient of correlation, τ, between X and Y is:

    $$ \theta = \sin \left( {\frac{{\pi \tau }}{2}} \right) $$
    (18)

Conditional copula

Let X and Y be random variables with marginal distribution as u = F X (x) and v = F Y (y). The conditional distribution function of X given Y = y can be expressed by the copula method as:

$$ \begin{array}{*{20}{c}} {H\left( {X < x\left| {Y = y} \right.} \right) = {{C}_{\theta }}\left( {u\left| {v = {{v}_{1}}} \right.} \right) = \mathop{{\lim }}\limits_{{\Delta v \to 0}} \frac{{{{C}_{\theta }}\left( {u,v + \Delta v} \right) - {{C}_{\theta }}\left( {u,v} \right)}}{{\Delta v}}} \\ { = \frac{\partial }{{\partial v}}{{C}_{\theta }}\left( {u,v} \right)\left| {v = {{v}_{1}}} \right.} \\ \end{array} $$
(19)

An equivalent formula for the conditional distribution function for Y given X = x can be obtained. The conditional distribution function of X given Y ≥ y can be expressed by the copula method as

$$ {{C}_{\theta }}\left( {u\left| {v < {{v}_{1}}} \right.} \right) = \frac{{{{C}_{\theta }}\left( {u,v} \right)}}{v} $$
(20)

Similarly, an equivalent formula for the conditional distribution function for Y given X < x can be obtained.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Zhang, Q., Xiao, M., Singh, V.P. et al. Copula-based risk evaluation of droughts across the Pearl River basin, China. Theor Appl Climatol 111, 119–131 (2013). https://doi.org/10.1007/s00704-012-0656-4

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00704-012-0656-4

Keywords

Navigation