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Evaporation from snow was calculated with the mean-profile method using single-level meteorological data at eight locations representing a variety of alpine and sub-alpine terrain in the central Sie...
The Dischma is a typical high mountain valley in the alpine source area of the River Rhine. A knowledge of the daily and seasonal water balance is important for understanding and predicting the effe...
By calculating the excess of the evaporation residue cross sections of the 200Pb nucleus over that predicted by the standard statistical model as a function of nuclear viscosity coefficient using a L...
On the Evaporation from the Northern Baltic.
Evaporation during the Spring Snowmelt Season.
A Computation of the Evaporation over Finland during a Rainless Period based on the Divergence of the Water-vapor Flux.
Computation of the Evaporation from the Baltic Sea from the Flux of Water Vapor in the Atmosphere
Using the Water-budget Method for the Determination of Evaporation from a Lake.
Estimating the Effect of Atmospheric Stability on Lake Evaporation with the Water Budget Method.
Estimation of Lake Evaporation by Using Different Aerodynamical Equations.
Annual water balances (1983-1995) for the Cwm and Delyn catchments at Llanbrynmair Moor in mid-Wales have been used to quantify the hydrological effects of the land use change in the Cwm from moorland...
Over the last decade there has been some uncertainty over the calculation of "actual" catchment evaporation from the long-term difference between rainfall and runoff for the grassland Wye catchment at...
The meteorological record from the manual Moel Cynnedd climate station at Plynlimon in the Welsh Uplands has been supplemented with solar radiation data, initially from the Institute of Hydrology's Do...
The Plynlimon experiment in mid-Wales, designed to determine the extent to which coniferous plantation increases evaporation losses and reduces streamflow relative to upland grassland, has now been yi...

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