Characterizing El Nino-Southern Oscillation Effects on the Blue Nile Yield and the Nile River Basin Precipitation using Empirical Mode Decomposition

被引:16
|
作者
Le, Justin A. [1 ]
El-Askary, Hesham M. [1 ,2 ,3 ]
Allali, Mohamed [1 ,4 ]
Sayed, Eman [5 ]
Sweliem, Hani [6 ,7 ]
Piechota, Thomas C. [1 ]
Struppa, Daniele C. [1 ]
机构
[1] Chapman Univ, Schmid Coll Sci & Technol, 1 Univ Dr, Orange, CA 92866 USA
[2] Chapman Univ, Ctr Excellence Earth Syst Modeling & Observat, Orange, CA 92866 USA
[3] Alexandria Univ, Dept Environm Sci, Fac Sci, Alexandria, Egypt
[4] Chapman Univ, Fowler Sch Engn, Orange, CA USA
[5] Egyptian Minist Water Resources & Irrigat, Cairo, Egypt
[6] Rhein Westfal TH Aachen, Dept Engn Hydrol, Aachen, Germany
[7] Amer Univ, Ctr Appl Res Environm & Sustainabil, Cairo, Egypt
关键词
ENSO effects; Nile river basin; El niñ o; Empirical mode decomposition; Southern oscillation index; Precipitation; VARIABILITY; ENSO; DROUGHT; FLOW;
D O I
10.1007/s41748-020-00192-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Using new mathematical and data-driven techniques, we propose new indices to measure and predict the strength of different El Nino events and how they affect regions like the Nile River Basin (NRB). Empirical Mode Decomposition (EMD), when applied to Southern Oscillation Index (SOI), yields three Intrinsic Mode Functions (IMF) tracking recognizable and physically significant non-stationary processes. The aim is to characterize underlying signals driving ENSO as reflected in SOI, and show that those signals also meaningfully affect other physical processes with scientific and predictive utility. In the end, signals are identified which have a strong statistical relationship with various physical factors driving ENSO variation. IMF 6 is argued to track El Nino and La Nina events occurrence, while IMFs 7 and 8 represent another signal, which reflects on variations in El Nino strength and variability between events. These we represent an underlying inter-annual variation between different El Nino events. Due to the importance of the latter, IMFs 7 and 8, are defined as Interannual ENSO Variability Indices (IEVI) and referred to as IEVI alpha and IEVI beta. EMD when applied to the NRB precipitation, affecting the Blue Nile yield, identifying the IEVI-driven IMFs, with high correlations of up to rho = 0.864, suggesting a decadal variability within NRB that is principally driven by interannual decadal-scale variability highlighting known geographical relationships. Significant hydrological processes, driving the Blue Nile yield, are accurately identified using the IEVI as a predictor. The IEVI-based model performed significantly at p = 0.038 with Blue Nile yield observations.
引用
收藏
页码:699 / 711
页数:13
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