Evaporation and energy balance of a wet grassland at Tadham Moor on the Somerset Levels
Version of Record online: 23 JAN 2008
Copyright © 2008 John Wiley & Sons, Ltd.
Volume 22, Issue 13, pages 2346–2357, 30 June 2008
How to Cite
Harding, R. J. and Lloyd, C. R. (2008), Evaporation and energy balance of a wet grassland at Tadham Moor on the Somerset Levels. Hydrol. Process., 22: 2346–2357. doi: 10.1002/hyp.6829
- Issue online: 31 MAY 2008
- Version of Record online: 23 JAN 2008
- Manuscript Accepted: 9 MAY 2007
- Manuscript Received: 27 JUN 2006
- Somerset Levels;
- water table;
- energy fluxes;
Wet grasslands are important both for their conservation value and for their important hydrological function. Evaporation is an important component of the water balance of a wetland. Where water is limited rainfall and/or surface (or sub-surface) inflows are required to balance the summer evaporation and thus become a significant factor in the maintenance and environmental health of a wetland. This study presents an almost complete year of measurements of the water and energy balance of a wet grassland in the Somerset Levels in southwest England. The majority of the radiant energy at this site goes into evaporation. There is a strong seasonality of the controls on evaporation; the roughness length varies by a factor of 10 between winter and summer. The surface resistance to evaporation is low, close to zero, during the winter when the water table is at, or just below the surface. In the summer the water table drops to 80 cm below the surface; there is no sign of soil water stress on the evaporation but a clear effect of the senescence of grass during seed head production and of the subsequent harvest. There is clear evidence that water for evaporation is provided by the drainage ditches through sub-surface flow. Standard evaporation formulae—such as the Penman-Monteith equation with constant and standard parameters—provide a reasonable simulation of the total evaporation at this site, although they miss some of the seasonal detail. Copyright © 2008 John Wiley & Sons, Ltd.