2018
DOI: 10.1002/2017wr021486
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Socio‐Hydrology of Channel Flows in Complex River Basins: Rivers, Canals, and Distributaries in Punjab, Pakistan

Abstract: This paper presents a socio‐hydrologic analysis of channel flows in Punjab province of the Indus River basin in Pakistan. The Indus has undergone profound transformations, from large‐scale canal irrigation in the mid‐nineteenth century to partition and development of the international river basin in the mid‐twentieth century, systems modeling in the late‐twentieth century, and new technologies for discharge measurement and data analytics in the early twenty‐first century. We address these processes through a s… Show more

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Cited by 45 publications
(21 citation statements)
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“…e IMF component reflects the nature and real information of the original time series. e instantaneous frequency of time series has a certain physical meaning after it is decomposed by the EMD method [29]. e EMD algorithm is suitable for complex time series of nonstationary and nonlinear data sequences.…”
Section: Complexitymentioning
confidence: 99%
“…e IMF component reflects the nature and real information of the original time series. e instantaneous frequency of time series has a certain physical meaning after it is decomposed by the EMD method [29]. e EMD algorithm is suitable for complex time series of nonstationary and nonlinear data sequences.…”
Section: Complexitymentioning
confidence: 99%
“…Wescoat et al () use historical geographic and statistical methods to gain context‐specific understanding of how and why measurements of water flows have been done in the ways they have in the Indus River Basin of Pakistan. They do their analysis in three levels of water channels: basin, canal, and local distributary levels.…”
Section: Contributions Of the Papers In The Special Section On Sociohmentioning
confidence: 99%
“…To thoroughly investigate the proposed models, four rivers' inflow data is used in this study which is comprised of daily rivers inflow (1 st -January to 19 th -June) for the period of 2015-2018. We consider the main river inflow of Indus at Tarbela with its two principal, one left and one right, bank tributaries [38]: Jhelum inflow at Mangla, Chenab at Marala, and Kabul at Nowshera, respectively (see Figure 4). Data is measured in 1000 cusecs.…”
Section: Case Study and Experimental Designmentioning
confidence: 99%