Summary
Plants play a dominating role in the evaporation of water from terrestrial systems. They act as a bridging mechanism in the transfer of water from soil to atmosphere. They thus lower the surface resistance to vapour exchange.
The Penman-Monteith combination equation is capable of describing the evaporation at the earth’s surface on the basis of the available energy, the meteorological conditions at some reference height — air temperature and vapour deficit — and two resistance parameters. It is applicable to almost any surface, at landscape scale and at leaf scale as well. It is sometimes used in simplified forms, such as the Priestly-Taylor equation. It can also be used as part of comprehensive multi layer models which can describe stomatal behaviour as function of environmental factors, micro-meteorological exchange within plant canopies or vertical patterns of soil water uptake and feed back mechanisms upon drought. Different modelling aims and different temporal and spatial scales generate the need for different model complexity.
Three types of models with different complexity are evaluated: Single Big Leaf models, SPAC models (Soil-Plant-Atmosphere Continuum) and Multi Layer models. Some soil water uptake models are also presented. Finally, rainfall interception models are discussed as the interception evaporation can be as high as half the precipitation amount and more than the transpiration on a yearly basis.
Several techniques are discussed for measuring the evaporation at different spatial scales including meteorological techniques to determine vapour fluxes above the canopy, the measurement of sap flow in plants, and the measurement of components of the water balance. Special attention is paid to the usefulness of these techniques in parametrizing and validating the various models.
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References
Aphalo P.J., Jarvis P.G. (1991) Do stomata respond to relative humidity? Plant Cell Environ., 14: 127–132.
Aussenac, G. (1970) Action du couvert forestier sur la distribution au sol des precipitations. Ann. Sci. For. 27: 383–399.
Ball J.T., Woodrow I.E., Berry J.A. (1987) A model predicting stomatal conductance and its contribution to the control of photosynthesis under different environmental conditions. In: Biggens Q(Ed.), Progress in Photosynthesis research. Vol. IV.: 221–225, Marinus Nijhoff, Dordrecht.
Barthakur N.N. (1983) The beta-ray gauge as a leaf wetness detector. Int. J. Appl. Radiat. Isot., 34:1549–1552.
Bosveld F.C., Bouten W., Noppert F. (1992) Transpiration dynamics of a Douglas fir forest II: Parametrisation of a Single Big Leaf model. In: W.Bouten, Monitoring and modelling forest hydrological processes in support of acidification research. PhD-thesis: 163–180, University of Amsterdam
Bouten W., Bosveld F.C. (1992a) Modelling rainfall interception and canopy wetness in a douglas fir stand. In: W. Bouten, Monitoring and modelling forest hydrological processes in support of acidification research. PhD-thesis: 65–88, University of Amsterdam.
Bouten W., Bosveld F.C. (1992b) Stomatal control in a partially wet Douglas fir canopy. In: W. Bouten, Monitoring and modelling forest hydrological processes in support of acidification research. PhD-thesis: 181–200, University of Amsterdam.
Bouten W., Bosveld F.C., Noppert F., Tiktak A. (1992a) Transpiration dynamics of a Douglas fir forest I: Evaluation of three measuring techniques. In: W. Bouten, Monitoring and modelling forest hydrological processes in support of acidification research. PhD-thesis: 149–161, University of Amsterdam.
Bouten W., Heimovaara T.J., Tiktak A. (1992b) Spatial patterns of soil water dynamics in a Douglas fir stand. Water Resources Research, vol.28, no. 12:3227–3233.
Bouten W., Swart P.J.F., de Water E. (1991) Microwave transmission, a new tool in forest hydrological research, J. Hydrol., 124, 119–130.
Bouten W., Schaap M.G., Aerts J.C.J.H., Vermetten A. (1994) Monitoring and modelling canopy water storage amounts in support of atmospheric deposition studies. J. Hydrol. (Submitted)
Businger J.A. (1986) Evaluation of the accuracy with which dry-deposition can be measured with current micro-meteorological techniques. Journal of Applied Meteorology (25):1100–1124.
Calder I.R. (1977) A model of transpiration and interception loss from a spruce forest in Plynlimon, central Wales. J. Hydrol. 33:247–275.
Calder I.R., Rosier P.T.W. (1976) The design of large plastic-sheet net rainfall gauges. J. Hydrol., 30: 403–405.
Calder I.R., Wright I.R. (1986) Gamma ray attenuation studies of interception from Sitka spruce: some evidence for an additional transport mechanism. Water Resour. Res., 22: 409–417.
Cassell D.K., Klute A. (1986) Water potential: Tensiometry. In: A. Klute (Ed.): Methods of soil analysis Part I, Physical and Mineralogical Methods 2th ed.: 563–569.
Cermâk J., Kucera J. (1981) The compensation of natural temperature gradients at the measuring point during sap flow rate determination in trees. Biol. Plant., 23: 469–471.
Cienciala E. (1994) Sap flow, transpiration and water use efficiency of spruce and willow in relation to climatic factors. PhD-thesis, Swe. Univ. Agric. Sci., ISSN 0348–422x.
Ford E.D., Deans J.D. (1978) The effect of canopy structure on stemflow, through-fall and interception loss in a young Sitka spruce plantation. J. Appl. Ecology, 15: 905–917.
Fritton D.D. (1969) Resolving time, mass absorption coefficient and water content with gamma-ray attenuation. Soil Science Society of America Proceedings, 33:651–655.
Gardner W.R. (1960) Dynamic aspects of water availability to plants. Soil Sci. 89: 63–73.
Gash J.H.C. (1979) An analytical model of rainfall interception by forests. Quart. J. R. Meteorol. Soc. 105: 43–55.
Gash J.H.C., Wright I.R., LLoyd C.R. (1980) Comparative estimates of interception loss from three coniferous forests in Great-Britain. J. Hydrol.. 48: 89–105.
Getz R.R. (1978) Dew monitoring network in the south east. Bull. Am. Meteor. Soc., 59: 1150–1154.
Goudriaan J. (1977) Crop micrometeorology: a simulation study, 249pp, Pudoc, Wageningen.
Granier A. (1985) Une nouvelle methode pour la mesure du flux seve brute dans le tronc des arbres. Ann. Sci. For., 42: 193–200.
Granier A. (1987) Mesure du flux de seve brute dans le tronc du Douglas par une nouvelle methode termique. Ann. Sci. For., 44: 1–14.
Halbertsma J., Przybyla C., Jacobs A. (1987) Application and accuracy of a dielectric soil water content meter. In: Proc. Conf. on measurement of soil and plant water status, Logan USA, 11–15, July 1987.
Hancock N.H., Crowther J.M. (1979) A technique for the direct measurement of water storage on a forest canopy. J. Hydrol., 41: 105–122.
Heimovaara T.J. (1994) Design of Triple Wire Time Domain Reflectometry Probes in Practice and Theory. Soil Sci. Soc. Am. J. 58: 1410–1417
Heimovaara T.J., Bouten W. (1990) A computer controlled 36-channel Time Domain Reflectometry system for monitoring soil water contents. Water Resources Research, 26:2311–2316.
Jackson I.J. (1975) Relationships between rainfall parameters and interception by tropical plant forests. J. Hydrol. 24:215–238.
Jarvis P.G. (1976) The interpretation of the variations in leaf water potential and stomatal conductance found in canopies in the field. Phil. Trans. R. Soc. Lond. B. (273):593–610.
Jones H.G. (1973) Estimation of plant water status with the beta gauge. Agric. Meteorol., 11: 345–355.
Kowalik P.J., Borghetti M., Busoni E., Sanesi G. (1988) Measured and simulated water relations in a Douglas-fir forest during the development of drought in the Apennines, Central Italy. For. Ecol. Manage. (25):181–194.
Lafolie F., Bruckler L., Tardieu F. (1991) Modeling root water potential and soil-root water transport: I: Model presentation. Soil Sci. Soc. Am. J. 55: 1203–1212.
Leadley P.W., Drake B.G. (1993) Open top chambers for exposing plant canopies to elevated CO, concentrations and for measuring net gas exchange. Vegetatio 104/105: 3–15.
Leuning R., Foster L.J. (1990) Estimation of transpiration by single trees: Comparison of a ventilated chamber, leaf energy budgets and a combination equation. Agric. and For. Meteorol. 51:63–68.
Lockwood J.G. (1992) The sensitivity of the water balance of a wet multi layer model pine canopy to variations in micrometeorological input, Clim. Change, 20, 23–56.
Lynn B.H., Carlson T.N. (1991) Simulating transpiration plateaus: the importance of leaf water potential. Ecol. Modelling, 58: 199–208.
Makkink G.F. (1957) Testing the Penman formula by means of lysimeters. Journ. Int. of Water Eng. 11: 277–288.
Marthaler H.P., Vogelsanger W., Richard F., Wierenga P.J. (1983) A pressure transducer for field tensiometers. Soil Science Society of America Journal, 47:624–627.
McKenney M.S., Rosenberg N.J. (1993) Sensitivity of some potential evapotranspiration estimation methods to climate change. Agric. For. Meteorol., 64: 81–110.
McNaughton K.G., Jarvis P.G. (1991) Effects of spatial scale on stomatal control of transpiration. Agric. For. Meteorol., 54: 279–301.
Monteith J.L. (1965) Evaporation and environment. In: The state and movement of water in living organisms. 19th Symp. Soc. Exp. Biol. (G.E. Fogg, ed.), pp205–235. Cambridge University Press, London.
Mott K.A., Parkhurst D.F. (1991) Stomata’ response to humidity in air and helox. Plant Cell Environm., 14, 509–515.
Mulder J.P.M. (1985) Simulating interception loss using standard meteorological data. In: Hutchison, B.A. and B.B. Hicks (eds), The forest-atmosphere interaction: 177–196, Reidel Publ. Comp.
Penman H.L. (1948) Natural evaporation from open water, bare soil and grass., Proc. Roy. Soc. London, Ser A, 193, pp120–146.
Priestley C.H.B., Taylor R.J. (1972) On the assessment of surface heat flux and evaporation using large scale parameters. Monthly Weather Review, 100, 2, pp 81–92.
Rawitz E., Etkin H., Hazan A. (1982) Calibration and field testing of a two-probe gamma-gauge. Soil Science Society of America Journal, 46:461–465.
Raupach M.R., Finnigan J.J. (1988) Single layer models of evaporation from plant canopies are incorrect, but useful, whereas multi layer models are correct but useless: Discuss. Aust. J. Plant Physiol., 15: 705–716
Rijtema P.E. (1965) An analysis of actual evapotranspiration. Agric. Res. Rep.659, Pudoc, Wageningen, The Netherlands.
Rutter A.J., Kershaw K.A., Robins P.C. and Morton A.J. (1971) A predictive model of rainfall interception in forests. I. Deviation of the model from observations in a plantation of Corsican Pine. Agric. Meteorol. 9:367–384.
Rutter A.J., Morton A.J., Robins P.C. (1975) A predictive model of rainfall interception in forests, II. Generalization of the model and comparison with observations in some coniferous and hardwood stands. J. Appl. Ecol., 12: 367–380.
Sakuratani T. (1981) A heat balance method for measuring water flux in the stem of intact plants. J. Agric. Meteorol., 37: 9–17.
Sellers P.J., Lockwood J.G. (1981) A computer simulation of the effects of differing crop types on the water balance of small catchments over long time periods. Quart. J. R. Meteorol. Soc. 107:395–414.
Schulze E.D., Cermâk J., Matyssek R., Penka M., Zimmerman R. (1985) Canopy transpiration and water fluxes in the xylem of the trunk of Larix and Picea trees - a comparison of xylem flow, porometer and cuvette measurements. Oecologia 66: 475–483.
Shuttleworth W.J. (1976) Experimental evidence for the failure of the PenmanMonteith equation in partly wet canopies. Boundary layer Meteorol., 10: 91–94.
Stewart J.B. (1988) Modelling surface conductance of pine forest. Agr. and Forest Met. (43):19–35.
Stewart J.B., Thom A.S. (1973) Energy budgets in a pine forest. Quart. J. Roy. Met. Soc., 103: 345–375.
Tan C.S., Black T.A. (1976) Factors affecting the canopy resistance of a Douglas-fir forest. Bound. Layer Met. (10):475–488.
Thom A.S., Oliver H.R. (1977) On Penman’s equation for estimating regional evaporation. Q.J.R. Meteorol. Soc., 103:345–357.
Tiktak A., Bouten W. (1992) Modelling soil water dynamics in a forested ecosystem III: model description and evaluation of discretization. Hydrol. Proc. 6: 455–465.
Topp G.C., Davis J.L., Annan A.P. (1980) Electromagnetic determination of soil water content: Measurements in coaxial transmission lines. Water Resources Research 16:574–582.
Wallin J.R. (1963) Dew, its significance and measurement in phytopathology. Phytopathology 53: 1210–1216.
Webb E.K., Pearman G.I., Leuning R. (1980) Corrections of flux measurements for density effects due to heat and water vapour transfer. Quart. J. Met. Soc. (106):85–100.
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Bouten, W. (1995). Plant Control on Evapotranspiration: Models and Measurements. In: Oliver, H.R., Oliver, S.A. (eds) The Role of Water and the Hydrological Cycle in Global Change. NATO ASI Series, vol 31. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-79830-6_4
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