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The relation between rain movement and areal reduction of rain intensity is investigated. An approach for calculating areal reduction factors from point hyetographs and storm speed is suggested. Ver...
Spatial variability in evapotranspiration from a crop covered field exposed to homogeneous climatic conditions is partly caused by field variability in soil physical properties and partly by field v...
While snowmelt and rain-on-snow events have received considerable attention in rural watersheds they have been largely ignored in urban hydrology, despite the fact that they may result in severe flo...
Swedish evaporation research has gone through a rapid development, and there is now a need to overview the results. This review presents the research in a broad sense. The brilliant research by Wall...
Public water supply in Europe relies very heavily on groundwater. Recharge of groundwater takes place mainly in the winter months. An analysis of winter rainfall data shows that current recharge rat...
Recent studies at Hot Weather Creek, Ellesmere Island document the climate and vegetation of a major part of the intermontane zone of Ellesmere Island. Summer temperatures in this region are much hi...
Extrapolating meteorological data to the basin scale represents a major problem of spatial snowmelt modelling in alpine terrain. Within this study errors in air temperature introduced by regionaliza...
A time-dependent cylindrically symmetric computer model of the Hofsjokull ice cap, Central Iceland, has been defined in order to investigate the time-scale of possible glacier variations. The model ...
Experiments were conducted with rainfall intensities of 45.0 and 140.0 mmlhr at slopes of 2, 9 and 20 per cent to separate the dominant effect of rainfall intensity on sediment transport capacity. T...
The Snowmelt-Runoff Model (SRM), a simple degree-day model, has been applied to over 50 basins in 15 countries around the world. Where results have been reported, the average R' has been 0.84 and th...
One of the most important consequences of future climate change may be an alteration of the surface hydrological balance, including changes in flow regimes, i.e. seasonal distribution of flow and es...
Sensitivity of streamflow simulations to changes in temperature and precipitation were evaluated for a small basin (A - 53 km2) characterized by low evapotranspiration and high conversion of precipi...
The aim of this article is to describe the seasonal fluctuations of suspended sediment yield in the Baltic Sea drainage basin and to quantify the monthly inflow of suspended sediment to the Baltic. ...
The aim of this paper is to quantify the spatial distribution of suspended sediment yield in the Baltic Sea drainage basin, and to quantify the suspended sediment inflow to the Baltic. The sediment ...
Possible consequences of climate change concern both changes in long-term mean values of runoff and changes in frequency and magnitude of extreme runoff events. The physical safety of dams and prote...

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