Paper No. JAWRA-11-0114-P of the Journal of the American Water Resources Association (JAWRA).Discussions are open until six months from print publication.
Modeling Monthly Fluctuations in Submersion Area of a Dammed River Reservoir: A Case Study1
Article first published online: 18 OCT 2012
© 2012 American Water Resources Association
JAWRA Journal of the American Water Resources Association
Volume 49, Issue 1, pages 90–102, February 2013
How to Cite
Lu, H., Li, S. S. and Guo, J. (2013), Modeling Monthly Fluctuations in Submersion Area of a Dammed River Reservoir: A Case Study. JAWRA Journal of the American Water Resources Association, 49: 90–102. doi: 10.1111/jawr.12003
- Issue published online: 4 FEB 2013
- Article first published online: 18 OCT 2012
- Received September 24, 2011; accepted August 20, 2012.
- open channel flow;
- environmental impacts;
- flooded area;
- backwater impoundment
Lu, Haorong, S. Samuel Li, and Jinsong Guo, 2012. Modeling Monthly Fluctuations in Submersion Area of a Dammed River Reservoir: A Case Study. Journal of the American Water Resources Association (JAWRA) 1-13. DOI: 10.1111/jawr.12003
Abstract: Fluctuations in water submersion of the Three Gorges Reservoir in China have not been explored in spite of their important implications for shoreline erosion and other undesirable consequences. This article aims to quantify the monthly fluctuations in response to changing hydraulic parameters and regional climatic factors. Flow velocity and water levels distributed along the 609-km long dammed river reservoir are calculated with a one-dimensional hydrodynamics model. Evaporation of water from the surface of the reservoir is determined using mass transfer-based methods. Calculated flow velocities and water levels compare well with field data. We show that the water surface slope decreases with rising water level at the dam, and decreases to almost zero during the winter months of water storage when the downstream water level reaches the normal pool level. The submersion area varies between 830 and 1,070 km2 over the year or over 20% of the reservoir zone will experience the annual cycle of dry land and partial or complete submersion. These fluctuations are of relevance to shoreline management and to the prevention and restoration of shoreline erosion. Evaporation is estimated to fluctuate between 1,240 and 26,110 tons of water per month per kilometer length of reservoir channel; this can possibly affect the hydrological budget of the reservoir region. The simple methodologies discussed in this article can easily be applied to other dammed river reservoirs for submersion estimates.