Land Surface Evaporation: Measurement and Parameterization ebook
Atmospheric Parameterization Schemes for Evaporation over Land: Basic Concepts and Climate Modeling Aspects. Parameterization Schemes of Land-Surface Processes for Mesoscale Atmospheric Models.
Atmospheric Parameterization Schemes for Evaporation over Land: Basic Concepts and Climate Modeling Aspects. Parameterization of Land-Surface Processes in Numerical Weather Prediction. Evaporation Models in Hydrology. Shuttleworth, W. James.
It will also give young scientists insight into surface processes. Thomas J. Schmugge, Jean-Claude Andre.
Evaporation Measurement. DOI: 1. 002/0470848944. In book: Encyclopedia of Hydrological Sciences. Cite this publication.
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Land Surface Evaporation - Measurement and Parameterization, Springer Verlag, S. 5-29.
In this study, the eddy covariance technique was used to measure net ecosystem CO2 exchange (NEE) of Alaskan wet sedge tundra and moist tussock tundra ecosystems during the summer (.
Evaporation is a cooling process- the latent heat of vapourisation (~585 cal/g of evaporated water) must be provided by the water body. Rate of evaporation depends on. Vapour pressures at the water surface and the air above. Wind speed – Incident solar radiation. Atmospheric pressure – Quality of water. Air and water temperatures. Vapour pressure – Rate of evaporation is proportional to the difference between the saturation vapour pressure (SVP) at the water temperature and the actual vapour pressure in the air ( ). This equation is called Dalton’s Law of Evaporation
Land surface in climate models Parameterization of surface fluxes Bart van den Hurk (KNMI/IMAU). Modeling of Actual Crop Water Consumption Using Optical-Thermal Satellite and Airborne Data Over Murrumbidgee Catchment Mohsin Hafeez, Shahbaz.
Land surface in climate models Parameterization of surface fluxes Bart van den Hurk (KNMI/IMAU). Evaluation of MODIS GPP product and scaling up GPP over Northern Australian savannas Kasturi Devi Kanniah Jason Beringer Lindsay Hutley Nigel Tapper Xuan.
The other type of vaporization is boiling, which is characterized by bubbles of saturated vapor forming in the liquid phase. Steam produced in a boiler is another example of evaporation occurring in a saturated vapor phase. Evaporation that occurs directly from the solid phase below the melting point, as commonly observed with ice at or below freezing or moth crystals (napthalene or paradichlorobenzene), is called sublimation.
The surface tensions have been measured based on the pendant droplet shape analysis. The Young–Laplace equation and the numerical model have been applied to precisely obtain surface tension from the balance between the droplet distortion of gravity and restoring the force of surface tension. The evaporation of the fuels has also been studied with pure droplets of a few millimeters in diameter in a ed environment.