Repository logo
  • Log In
    Log in via Symplectic to deposit your publication(s).
Repository logo
  • Communities & Collections
  • Research Outputs
  • Statistics
  • Log In
    Log in via Symplectic to deposit your publication(s).
  1. Home
  2. Faculty of Engineering
  3. Faculty of Engineering
  4. Temporal scaling phenomena in groundwater-floodplain systems using robust detrended fluctuation analysis
 
  • Details
Temporal scaling phenomena in groundwater-floodplain systems using robust detrended fluctuation analysis
File(s)
Habib+_JH2017_Temporal scaling phenomena in groundwater-floodplain systems using rDFA_submitted.pdf (1.71 MB)
Accepted version
Author(s)
Habib, A
Sorensen, JPR
Bloomfield, JP
Muchan, K
Newell, AJ
more
Type
Journal Article
Abstract
In order to determine objectively the fractal behaviour of a time series, and to facilitate potential future attempts to assess model performance by incorporating fractal behaviour, a multi-order robust detrended fluctuation analysis (r-DFAn) procedure is developed herein. The r-DFAn procedure allows for robust and automated quantification of mono-fractal behaviour. The fractal behaviour is quantified with three parts: a global scaling exponent, crossovers, and local scaling exponents. The robustness of the r-DFAn procedure is established by the systematic use of robust regression, piecewise linear regression, Analysis of Covariance (ANCOVA) and Multiple Comparison Procedure to determine statistically significant scaling exponents and optimum crossover locations. The MATLAB code implementing the r-DFAn procedure has also been open sourced to enable reproducible results.

r-DFAn will be illustrated on a synthetic signal after which is used to analyse high-resolution hydrologic data; although the r-DFAn procedure is not limited to hydrological or geophysical time series. The hydrological data are 4 year-long datasets (January 2012 to January 2016) of 1-min groundwater level, river stage, groundwater and river temperature, and 15-min precipitation and air temperature, at Wallingford, UK. The datasets are analysed in both time and fractal domains. The study area is a shallow riparian aquifer in hydraulic connection to River Thames, which traverses the site. The unusually high resolution datasets, along with the responsive nature of the aquifer, enable detailed examination of the various data and their interconnections in both time- and fractal-domains.
Date Issued
2017-04-18
Date Acceptance
2017-04-14
Citation
Journal of Hydrology, 2017, 549, pp.715-730
URI
http://hdl.handle.net/10044/1/49567
DOI
https://www.dx.doi.org/10.1016/j.jhydrol.2017.04.034
ISSN
0022-1694
Publisher
Elsevier
Start Page
715
End Page
730
Journal / Book Title
Journal of Hydrology
Volume
549
Copyright Statement
© 2017 Elsevier B.V. All rights reserved. This manuscript is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/licenses/by-nc-nd/4.0/
Identifier
http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000403855500055&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=1ba7043ffcc86c417c072aa74d649202
Subjects
Science & Technology
Technology
Physical Sciences
Engineering, Civil
Geosciences, Multidisciplinary
Water Resources
Engineering
Geology
Robust detrended fluctuation analysis
Detrended fluctuation analysis
Fractal behaviour
Hurst Phenomenon
Time series analysis
High resolution hydrological data
LONG-RANGE CORRELATIONS
TIME-SERIES
RAINFALL
MULTIFRACTALITY
STREAMFLOW
AQUIFERS
Publication Status
Published
About
Spiral Depositing with Spiral Publishing with Spiral Symplectic
Contact us
Open access team Report an issue
Other Services
Scholarly Communications Library Services
logo

Imperial College London

South Kensington Campus

London SW7 2AZ, UK

tel: +44 (0)20 7589 5111

Accessibility Modern slavery statement Cookie Policy

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science

  • Cookie settings
  • Privacy policy
  • End User Agreement
  • Send Feedback