Evaluating Performance and Applicability of Several Drought Indices in Arid Regions

被引:29
作者
Moghimi, Mohammad Mehdi [1 ]
Zarei, Abdol Rassoul [2 ]
机构
[1] Fasa Univ, Coll Agr, Dept Water Sci Engn, Fasa, Iran
[2] Fasa Univ, Coll Agr, Dept Range & Watershed Management Nat Engn, Fasa, Iran
关键词
Reconnaissance drought index; Generalized estimating equations; Drought; Iran; RDI simulation; STANDARDIZED PRECIPITATION INDEX; GENERALIZED ESTIMATING EQUATIONS; RDI; GEE;
D O I
10.1007/s13143-019-00122-z
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Drought is a complex phenomenon that strong indices should be used to quantifying it. Reconnaissance drought index (RDI) is very strong index that extensively used in drought investigating researches. Major problem to calculate this index especially in arid and semi-arid regions at undeveloped countries is lack of data for calculating evapotranspiration. This study investigated this problem(')s solution via simulating monthly RDI using other indices (PN, DI, SPI, CZI, MCZI and Z-Score) that in order to calculate these indices, only precipitation data is used. To simulate RDI, Generalized Estimating Equations (GEE) was used. For validation of estimating equations, different indices of goodness of fit were used (NSE, RMSE, MAE, R-2, QIC and QICC). Results of this study indicated that the SPI, CZI, MCZI and DI indices had the most appropriateness for simulating RDI. When the SPI index (the best index for simulating RDI) was used to simulate the RDI, according to the results of T-Test, the observed and simulated data series hadn't significantly difference (P value >0.05) in all stations. The average values of NSE, R-2, RMSE, MAE, QIC and QICC obtained 0.976, 0.139, 0.088, 0.976, 21.24 and 17.82 sequential.
引用
收藏
页码:645 / 661
页数:17
相关论文
共 38 条
  • [1] [Anonymous], 2004, 83 INT WAT MAN I
  • [2] [Anonymous], 2014, Natural Hazards and Earth System Sciences Discussions, DOI [DOI 10.5194/NHESSD-2-2245-2014, DOI 10.5194/nhessd-2-2245-2014]
  • [3] Using generalized estimating equations for longitudinal data analysis
    Ballinger, GA
    [J]. ORGANIZATIONAL RESEARCH METHODS, 2004, 7 (02) : 127 - 150
  • [4] Factors Influencing Markov Chains Predictability Characteristics, Utilizing SPI, RDI, EDI and SPEI Drought Indices in Different Climatic Zones
    Banimahd, Seyed Adib
    Khalili, Davar
    [J]. WATER RESOURCES MANAGEMENT, 2013, 27 (11) : 3911 - 3928
  • [5] Bennani S., 2017, Australian Journal of Crop Science, V11, P395, DOI 10.21475/ajcs.17.11.04.pne272
  • [6] Drought forecasting using the standardized precipitation index
    Cancelliere, A.
    Di Mauro, G.
    Bonaccorso, B.
    Rossi, G.
    [J]. WATER RESOURCES MANAGEMENT, 2007, 21 (05) : 801 - 819
  • [7] Long-term spatio-temporal drought variability in Turkey
    Dabanli, Ismail
    Mishra, Ashok K.
    Sen, Zekai
    [J]. JOURNAL OF HYDROLOGY, 2017, 552 : 779 - 792
  • [8] Drought Forecasting Using Neural Networks, Wavelet Neural Networks, and Stochastic Models: Case of the Algerois Basin in North Algeria
    Djerbouai, Salim
    Souag-Gamane, Doudja
    [J]. WATER RESOURCES MANAGEMENT, 2016, 30 (07) : 2445 - 2464
  • [9] Gabriele B., 2017, MEASUREMENT, V113, P205
  • [10] Fixed effects, random effects and GEE: What are the differences?
    Gardiner, Joseph C.
    Luo, Zhehui
    Roman, Lee Anne
    [J]. STATISTICS IN MEDICINE, 2009, 28 (02) : 221 - 239