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-List Of Titles -Comparative assessment of three approaches for deriving stream power plots along long profiles in the upper Hunter River catchment, New South Wales, Australia

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/7951

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Title
Comparative assessment of three approaches for deriving stream power plots along long profiles in the upper Hunter River catchment, New South Wales, Australia
Related
Geomorphology, Vol. 74, Issue 1-4, p.297-317
DOI
10.1016/j.geomorph.2005.08.012
Publisher
Elsevier
Date
2006
Author/Creator
Jain, Vikrant
Author/Creator
Preston, Nicholas
Author/Creator
Fryirs, Kirstie
Author/Creator
Brierley, Gary
Description
The downstream distribution of stream power is derived and analysed for 11 different streams in the upper Hunter River catchment, Australia. Stream long profiles were produced in a GIS environment using DEM data and catchment area–discharge analysis. These profiles were analysed using three approaches, namely long profile smoothing, curve fitting and a theoretical model. The methodology for deriving stream power profiles using these three approaches is discussed. The long profile smoothing method provides a good approximation of the subcatchment variability in stream power trends. The curve fitting method shows that higher-order exponential curves provide a better fit for long profile data. For the streams of the upper Hunter River catchment, second-order exponential curves fit well with significantly less error. The curve fitting method predicts a bimodal (upstream and midstream) distribution of stream power, which is a deviation from our earlier understanding of a single midstream peak. The theoretical approach provides a mathematical expression of the observed bimodal stream power distribution. The bimodal distribution emphasises the erosion potential of headwater reaches. The resultant stream power distribution provides a catchment-scale characterisation of the distribution of available energy in any given system. Using these approaches, the variability of stream power in headwater reaches is explained by discharge variability, while variability in midstream and downstream reaches is related to high variability in channel gradient.
Description
21 page(s)
Subject Keyword
stream power
Subject Keyword
energy distribution
Subject Keyword
DEM
Subject Keyword
long profile
Subject Keyword
New South Wales
Resource Type
journal article
Organisation
Macquarie University. Dept. of Physical Geography

Identifier
http://hdl.handle.net/1959.14/7951
Identifier
ISSN:1872-695X
Identifier
mq-rm-2006001225
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Geomorphology"
 
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