Comparison of Models for Calculation of Diel Sediment-Water Heat Flux from Water Temperatures
This article has been corrected.
VIEW CORRECTIONPublication: Journal of Hydraulic Engineering
Volume 137, Issue 10
Abstract
We investigated sediment-water heat flux estimation in relation to applications (hydrodynamics simulation, evaporation studies, or global change effects assessment) in which sediment temperatures are not available because of technical complications (difficulties in installing sensors, for example) or because of methodology used (remote sensing, for example). We used field sediment temperature data measured every 10 min to 1 m depth at Doñana National Park marshland to obtain sediment thermal properties and to calculate diel sediment-water heat exchange through Beck’s sequential function specification method. We compare four models for the simulation of sediment-water heat flux by using surface temperatures. Two models need initial estimated inside sediment temperatures; the other two do not. Influence of estimated initial temperature profiles depends on the temperature distribution assumption and is significant for three days or fewer at the daily timescale. A model that does not use initial sediment temperatures provides accurate estimations with low computation time.
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Acknowledgments
The authors would like to thank Doñana National Park and the Estación Biológica de Doñana for assisting with installing instrumentation. The authors would also like to acknowledge the work of Quim Rabadà and Daniel Niñerola in maintaining and installing field instrumentation. This study was funded by the Ministerio de Educación y Cultura (complementary action UNSPECIFIEDCMT2007-30881-E/TECNO), by the 6th Framework Program of the European Union (contract EUGOCE-CT-2006-037081), and by the Confederación Hidrográfica del Guadalquivir.
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© 2011 American Society of Civil Engineers.
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Received: Jul 12, 2010
Accepted: Apr 1, 2011
Published online: Apr 4, 2011
Published in print: Oct 1, 2011
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