RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site

This paper compares direct measurements of evaporation with the values predicted for reference transpiration. The measurements of actual evaporation were made using an eddy correlation device on a grass field adjacent to the river Thames. Measurements of soil moisture and the driving meteorological...

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Main Authors: J. W. Finch, R. J. Harding
Format: Article
Language:English
Published: Copernicus Publications 1998-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/2/129/1998/hess-2-129-1998.pdf
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author J. W. Finch
R. J. Harding
author_facet J. W. Finch
R. J. Harding
author_sort J. W. Finch
collection DOAJ
description This paper compares direct measurements of evaporation with the values predicted for reference transpiration. The measurements of actual evaporation were made using an eddy correlation device on a grass field adjacent to the river Thames. Measurements of soil moisture and the driving meteorological variables were also made. The results showed that, during a period with minimal rainfall but no water stress, the cumulative values of reference transpiration compared very well with the cumulative measured evaporation and changes in soil moisture content. However, the values on specific days did not compare well. Following significant rainfall, the measured evaporation increased for a few days, probably due to evaporation of free water from the canopy or soil. Reference transpiration fell consistently below the measured evaporation once the soil moisture deficits exceeded 140 to 150 mm.
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spelling doaj.art-b814d42ef4464770863f782efbb9d23d2022-12-22T01:38:00ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79381998-01-0121129136RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland siteJ. W. FinchR. J. HardingThis paper compares direct measurements of evaporation with the values predicted for reference transpiration. The measurements of actual evaporation were made using an eddy correlation device on a grass field adjacent to the river Thames. Measurements of soil moisture and the driving meteorological variables were also made. The results showed that, during a period with minimal rainfall but no water stress, the cumulative values of reference transpiration compared very well with the cumulative measured evaporation and changes in soil moisture content. However, the values on specific days did not compare well. Following significant rainfall, the measured evaporation increased for a few days, probably due to evaporation of free water from the canopy or soil. Reference transpiration fell consistently below the measured evaporation once the soil moisture deficits exceeded 140 to 150 mm.http://www.hydrol-earth-syst-sci.net/2/129/1998/hess-2-129-1998.pdf
spellingShingle J. W. Finch
R. J. Harding
RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
Hydrology and Earth System Sciences
title RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
title_full RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
title_fullStr RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
title_full_unstemmed RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
title_short RESEARCH NOTE<br>A comparison between reference transpiration and measurements of evaporation for a riparian grassland site
title_sort research note br a comparison between reference transpiration and measurements of evaporation for a riparian grassland site
url http://www.hydrol-earth-syst-sci.net/2/129/1998/hess-2-129-1998.pdf
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