Prediction of the impact of climate change on drought: an evaluation of six UK catchments using two stochastic approaches

被引:27
作者
Chun, Kwok Pan [1 ]
Wheater, Howard [1 ]
Onof, Christian [1 ]
机构
[1] Univ London Imperial Coll Sci Technol & Med, Dept Civil & Environm Engn, London SW7 2AZ, England
关键词
drought; generalized linear model (GLM); autoregressive integrated moving average (ARIMA); extremes; persistence; forecast; AGRICULTURAL DROUGHT; DAILY PRECIPITATION; FUTURE CLIMATE; DAILY RAINFALL; EL-NINO; MODEL; SEVERITY; METHODOLOGY; OSCILLATION; VARIABILITY;
D O I
10.1002/hyp.9259
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Under future climate scenarios, possible changes of drought patterns pose new challenges for water resources management. For quantifying and qualifying drought characteristics in the UK, the drought severity indices of six catchments are investigated and modelled by two stochastic methods: autoregressive integrated moving average (ARIMA) models and the generalized linear model (GLM) approach. From the ARIMA models, autocorrelation structures are first identified for the drought index series, and the unexplained variance of the series is used to establish empirical relationships between drought and climate variables. Based on the ARIMA results, mean sea level pressure and possibly the North Atlantic Oscillation index are found to be significant climate variables for seasonal drought forecasting. Using the GLM approach, occurrences and amounts of rainfall are simulated with conditioning on climate variables. From the GLM-simulated rainfall for the 1980s and 2080s, the probabilistic characteristics of the drought severity are derived and assessed. Results indicate that the drought pattern in the 2080s is less certain than for the 19611990 period, based on the Shannon entropy, but that droughts are expected to be more clustered and intermittent. The 10th and 50th quantiles of drought are likely higher in the 2080s scenarios, but there is no evidence showing the changes in the 90th quantile extreme droughts. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:1600 / 1614
页数:15
相关论文
共 102 条
[21]  
[Anonymous], CLIM CHANG AD TOM
[22]  
[Anonymous], WATER RESOURCES RES
[23]  
BARDSLEY P, 1984, AUST J AGR ECON, V28, P1
[24]   Multi-indices analysis of southern Scandinavian storminess 1780-2005 and links to interdecadal variations in the NW Europe-North Sea region [J].
Barring, Lars ;
Fortuniak, Krzysztof .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2009, 29 (03) :373-384
[25]  
Bates B.C., 2008, LINKING CLIMATE CHAN
[26]   Changes in drought frequency, severity and duration for the British Isles projected by the PRUDENCE regional climate models [J].
Blenkinsop, S. ;
Fowler, H. J. .
JOURNAL OF HYDROLOGY, 2007, 342 (1-2) :50-71
[27]  
Bryant S., 1992, P IWEM C MAN SCARC W
[28]  
BRYANT SJ, 1994, J INST WATER ENV MAN, V8, P39
[29]   An historical record of evaporation losses since 1815 calculated using long-term observations from the Radcliffe Meteorological Station, Oxford, England [J].
Burt, TP ;
Shahgedanova, M .
JOURNAL OF HYDROLOGY, 1998, 205 (1-2) :101-111
[30]   Drought length properties for periodic-stochastic hydrologic data [J].
Cancelliere, A ;
Salas, JD .
WATER RESOURCES RESEARCH, 2004, 40 (02)