Review of complex networks application in hydroclimatic extremes with an implementation to characterize spatio-temporal drought propagation in continental USA

被引:100
作者
Konapala, Goutam [1 ]
Mishra, Ashok [1 ]
机构
[1] Clemson Univ, Glenn Dept Civil Engn, Clemson, SC 29634 USA
基金
美国国家科学基金会;
关键词
Complex networks; Event synchronization; Network theory; Extreme events; Drought; FLOOD FREQUENCY-ANALYSIS; UNITED-STATES; CLIMATE; PRECIPITATION; MODEL; RAINFALL; TIME; TEMPERATURE; VARIABILITY; FRAMEWORK;
D O I
10.1016/j.jhydrol.2017.10.033
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The quantification of spatio-temporal hydroclimatic extreme events is a key variable in water resources planning, disaster mitigation, and preparing climate resilient society. However, quantification of these extreme events has always been a great challenge, which is further compounded by climate variability and change. Recently complex network theory was applied in earth science community to investigate spatial connections among hydrologic fluxes (e.g., rainfall and streamflow) in water cycle. However, there are limited applications of complex network theory for investigating hydroclimatic extreme events. This article attempts to provide an overview of complex networks and extreme events, event synchronization method, construction of networks, their statistical significance and the associated network evaluation metrics. For illustration purpose, we apply the complex network approach to study the spatio-temporal evolution of droughts in Continental USA (CONUS). A different drought threshold leads to a new drought event as well as different socio-economic implications. Therefore, it would be interesting to explore the role of thresholds on spatio-temporal evolution of drought through network analysis. In this study, long term (1900-2016) Palmer drought severity index (PDSI) was selected for spatio-temporal drought analysis using three network-based metrics (i.e., strength, direction and distance). The results indicate that the drought events propagate differently at different thresholds associated with initiation of drought events. The direction metrics indicated that onset of mild drought events usually propagate in a more spatially clustered and uniform approach compared to onsets of moderate droughts. The distance metric shows that the drought events propagate for longer distance in western part compared to eastern part of CONUS. We believe that the network-aided metrics utilized in this study can be an important tool in advancing our knowledge on drought propagation as well as other hydroclimatic extreme events. Although the propagation of droughts is investigated using the network approach, however process (physics) based approaches is essential to further understand the dynamics of hydroclimatic extreme events. (c) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:600 / 620
页数:21
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