Loughborough University
Leicestershire, UK
LE11 3TU
+44 (0)1509 263171
Loughborough University

Loughborough University Institutional Repository

Please use this identifier to cite or link to this item: https://dspace.lboro.ac.uk/2134/23995

Title: Imprint of climate and climate change in alluvial riverbeds: Continental United States, 1950-2011
Authors: Slater, Louise
Singer, Michael Bliss
Issue Date: 2013
Publisher: © Geological Society of America
Citation: SLATER, L. and SINGER, M.B., 2013. Imprint of climate and climate change in alluvial riverbeds: Continental United States, 1950-2011. Geology, 41(5), pp. 595-598.
Abstract: Alluvial riverbed elevation responds to the balance between sediment supply and transport capacity, which is largely dependent on climate and its translation into fluvial discharge. We examine these relations using U.S. Geological Survey streamflow and channel measurements in conjunction with basin characteristics for 915 reference (“least disturbed”) measurement stations across the conterminous United States for the period A.D. 1950–2011. We find that (1) 68% of stations have bed elevation change (BEC) trends (p < 0.05) with median values of +0.5 cm/yr for aggradation and –0.6 cm/yr for degradation, with no obvious relation to drainage basin structure, physiography, or lithology; (2) BEC correlates with drainage basin area; (3) high-flow variability (Q90/Q50, where Q is discharge and 90 and 50 are annual flow percentiles) translates directly into the magnitude, though not the direction, of BEC, after accounting for the scale dependence; (4) Q90/Q50 declines systematically from dry to wet climates, producing disproportionately high rates of BEC in drier regions; and (5) marked increases in precipitation and streamflow occurred disproportionately at dry sites, while streamflow declined disproportionately at wet sites. Climatic shifts in streamflow have the potential to increase/decrease sediment flux and thus affect riverbed elevation by altering flood frequency. These unforeseen responses of bed elevation to climate and climate change have important implications for sediment budgets, longitudinal profiles, ecology, and river management.
Description: This paper was accepted for publication in the journal Geology and the definitive published version is available at http://dx.doi.org/10.1130/G34070.1
Version: Accepted for publication
DOI: 10.1130/G34070.1
URI: https://dspace.lboro.ac.uk/2134/23995
Publisher Link: http://dx.doi.org/10.1130/G34070.1
ISSN: 0091-7613
Appears in Collections:Published Articles (Geography)

Files associated with this item:

File Description SizeFormat
Slater_G34070_7.30pm_final upload_short.pdfAccepted version10.29 MBAdobe PDFView/Open

 

SFX Query

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.