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Related Concept Videos

Rapidly Varying Flow01:24

Rapidly Varying Flow

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Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
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End Point Prediction: Gran Plot01:07

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A Gran plot is used to predict the equivalence volume or endpoint of a potentiometric or acid-base titration without reaching the endpoint. Typically, titration data is collected as a function of the titrant's volume up to a point less than the equivalence volume and then transformed into a linear format. The straight line is extended to the x-axis, indicating the necessary titrant volume to achieve the equivalence point.
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Sequence Networks of Rotating Machines01:24

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A Y-connected synchronous generator, grounded through a neutral impedance, is designed to produce balanced internal phase voltages with only positive-sequence components. The generator's sequence networks include a source voltage that is exclusively in the positive-sequence network. The sequence components of line-to-ground voltages at the generator terminals illustrate this configuration.
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Gradually Varying Flow01:29

Gradually Varying Flow

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Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
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Signal Flow Graphs01:18

Signal Flow Graphs

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Signal-flow graphs offer a streamlined and intuitive approach to representing control systems, providing an alternative to traditional block diagrams. These graphs use branches to symbolize systems and nodes to represent signals, effectively illustrating the relationships and interactions within the system.
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Uniform Depth Channel Flow: Problem Solving01:18

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To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...
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Spatial Temporal Analysis of Fieldwise Flow in Microvasculature
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Streamflow Prediction Using Complex Networks.

Abdul Wajed Farhat1, B Deepthi1, Bellie Sivakumar1

  • 1Department of Civil Engineering, Indian Institute of Technology Bombay, Powai, Mumbai 400 076, India.

Entropy (Basel, Switzerland)
|July 26, 2024
PubMed
Summary

This study introduces a novel complex networks approach for streamflow prediction. The method uses streamflow data to build networks and predict future flows, showing promising results across the contiguous United States.

Keywords:
clustering coefficientcoefficient of variationcontiguous United Statesdistance thresholdnearest neighbor approachnetwork theory

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Area of Science:

  • Hydrology and Water Resources Engineering
  • Complex Systems Analysis
  • Time Series Forecasting

Background:

  • Reliable streamflow prediction is essential for water resource management, environmental monitoring, and ecosystem health.
  • Existing streamflow prediction methods often face challenges in capturing complex temporal dynamics.
  • Complex networks offer a novel framework for analyzing and modeling time series data.

Purpose of the Study:

  • To develop and evaluate a complex networks-based approach for daily streamflow prediction.
  • To assess the prediction accuracy using established statistical metrics.
  • To investigate the relationship between prediction accuracy and catchment characteristics.

Main Methods:

  • Streamflow time series were transformed into complex networks where timesteps are nodes and streamflow differences define links.
  • A critical distance threshold was identified to form the network structure.
  • Clustering coefficient (CC) was calculated and used in a nearest neighbor search for prediction.

Main Results:

  • The complex networks approach was applied to 142 stations in the contiguous United States, yielding prediction accuracies with correlation coefficients (R) from 0.05 to 0.99.
  • Normalized root mean square error (NRMSE) ranged from 0.1 to 12.3, and Nash-Sutcliffe efficiency (NSE) ranged from -0.89 to 0.99.
  • Prediction accuracy showed a stronger relationship with the coefficient of variation of flow than with drainage area or mean flow.

Conclusions:

  • The proposed complex networks-based method provides a promising tool for accurate streamflow prediction.
  • The approach demonstrates effective application across diverse hydrological conditions in the United States.
  • Further research can extend this methodology to other hydrologic time series forecasting applications.