A composite index coupling five key elements of water cycle for drought analysis in Pearl River basin, China

被引:17
作者
Wang, Tian [1 ]
Tu, Xinjun [1 ,2 ,3 ]
Singh, Vijay P. [4 ,5 ,6 ]
Chen, Xiaohong [1 ]
Lin, Kairong [1 ]
机构
[1] Sun Yat Sen Univ, Ctr Water Resources & Environm, Sch Civil Engn, Guangzhou 510275, Peoples R China
[2] Ctr Water Secur Engn & Technol Southern China Guan, Guangzhou 510275, Peoples R China
[3] Guangdong Lab Southern Ocean Sci & Engn, Zhuhai 519000, Peoples R China
[4] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[5] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX 77843 USA
[6] UAE Univ, Natl Water & Energy Ctr, Al Ain, U Arab Emirates
基金
中国国家自然科学基金;
关键词
Drought; Standardized water cycle index; D-vine copula; Kendall distribution transform; CMIP6; Pearl river basin; CLIMATE-CHANGE; SOIL-MOISTURE; METEOROLOGICAL DROUGHT; VEGETATION; COPULA; MODEL; IDENTIFICATION; SIMULATIONS; EXTREMES; EVENTS;
D O I
10.1016/j.jenvman.2022.115813
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Drought, as a natural disaster, has widespread consequences and is notoriously difficult to manage. Critical to developing a drought management strategy is the identification and assessment of drought. To that end, this study developed a new composite index, called the standardized water cycle index (SWCI) based on the water cycle and water balance. The SWCI couplesd the key elements of the water cycle, including precipitation, evapotranspiration, leaf area index, surface runoff, and subsurface runoff, and requires the joint distribution of these elements which was determined using the D-vine copula. The Kendall transform was used to reduce the dimensionality of the five-element joint probability density function, which was then inversed to obtain the SWCI which was then evaluated with the data from the Pearl River basin obtained using the CMIP6. Results showed that the SWCI satisfactorily evaluated drought conditions, while reflecting the drought-mitigating effect of vegetation and subsurface runoff. The SWCI was also able to evaluate drought in areas with a high level of human activity.
引用
收藏
页数:14
相关论文
共 71 条
[1]   FACTOR-ANALYSIS AND AIC [J].
AKAIKE, H .
PSYCHOMETRIKA, 1987, 52 (03) :317-332
[2]   An Intercomparison of Drought Indicators Based on Thermal Remote Sensing and NLDAS-2 Simulations with US Drought Monitor Classifications [J].
Anderson, Martha C. ;
Hain, Christopher ;
Otkin, Jason ;
Zhan, Xiwu ;
Mo, Kingtse ;
Svoboda, Mark ;
Wardlow, Brian ;
Pimstein, Agustin .
JOURNAL OF HYDROMETEOROLOGY, 2013, 14 (04) :1035-1056
[3]  
Baba R., 2013, J ARID METEOROL, V27, P4
[4]  
Bedford T, 2002, ANN STAT, V30, P1031
[5]   Soil moisture estimation through ASCAT and AMSR-E sensors: An intercomparison and validation study across Europe [J].
Brocca, L. ;
Hasenauer, S. ;
Lacava, T. ;
Melone, F. ;
Moramarco, T. ;
Wagner, W. ;
Dorigo, W. ;
Matgen, P. ;
Martinez-Fernandez, J. ;
Llorens, P. ;
Latron, J. ;
Martin, C. ;
Bittelli, M. .
REMOTE SENSING OF ENVIRONMENT, 2011, 115 (12) :3390-3408
[6]   The Vegetation Drought Response Index (VegDRI): A new integrated approach for monitoring drought stress in vegetation [J].
Brown, Jesslyn F. ;
Wardlow, Brian D. ;
Tadesse, Tsegaye ;
Hayes, Michael J. ;
Reed, Bradley C. .
GISCIENCE & REMOTE SENSING, 2008, 45 (01) :16-46
[7]  
Chambers J. M., 1983, Graphical Methods for Data Analysis
[8]   Copula-based method for multisite monthly and daily streamflow simulation [J].
Chen, Lu ;
Singh, Vijay P. ;
Guo, Shenglian ;
Zhou, Jianzhong ;
Zhang, Junhong .
JOURNAL OF HYDROLOGY, 2015, 528 :369-384
[9]   Precipitation extremes estimated by GPCP and TRMM: ENSO relationships [J].
Curtis, Scott ;
Salahuddin, Ahmed ;
Adler, Robert F. ;
Huffman, George J. ;
Gu, Guojun ;
Hong, Yang .
JOURNAL OF HYDROMETEOROLOGY, 2007, 8 (04) :678-689
[10]   Drought under global warming: a review [J].
Dai, Aiguo .
WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE, 2011, 2 (01) :45-65