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In the last decades, an increase in the number of extreme precipitation events has been observed, which leads to increasing risks for flash floods and landslides. Thereby, conventional gauging station...
Through the rapid development in the field of electrotechniques and the development ot highly sophisticated recision components it has been possible to design a new simplified electrical instrumcnt ...
An account is given of precipitation measurements taken with various precipitation gauge installations at Ultuna, Sweden during 1957-1960. A new gauge constructed to measure small spatial variations...
Measurcmcnts on evaporation and the melting of snow cover are presented, followed by .an explanation of how the measured values depend on mctcorological factors and thc structure of the snow. The ob...
The effect of gauge height, exposure and screening on systematic errors in rainfall estimation is investigated. Adhesion losses are found to be more than 2% of the annual precipitation, but for summ...
The normal-exposed Hellmann raingauge only catches about 85% of the true precipitation on yearly basis. This is mainly due to aerodynamic effects. A statistical model analysing the ratio of the dail...
Water discharges in small turbulent streams are determined by injecting concentrated salt solutions at constant feed-rate and measuring the dilution level downstream by conductivity readings in situ...
Possible evaporation rates from a snow surface with respect to available energy and vapour pressure deficit in the air are discussed. In literature reported measurements and measurements carried out...
Prior microwave measurements of snow water equivalent and liquid water content and conceptualizations of emission and backscattering models are reviewed. The results of an experiment designed to col...
The snow cover is an important parameter for water run-off prediction in high mountain areas. At present its seasonal changes can be monitored regularly by satellite. The paper presents a new method...
From 1969 to 1980, each March, snow depth and water equivalent were sampled around 249 pins of a grid covering the forested portion of Marmot Creek basin. Continuous record from four snow pillows an...
The inversion of snow water equivalent, SWE, from passive microwave remote sensing measurements may be accomplished by using a neural network trained with a dense media multiple scattering model. Br...
The paper describes a measurement project aiming at delivering water quality data with the very fine time resolution necessary to discover deterministic elements of the complex process of pollution ...
The paper aims at relating the discharge through 0resund (the sound between Denmark and Sweden) to measured current and stratification at the two fixed stations Nordre Rese (St. 24) and Flinten SW (...
The river Bayelva drains a catchment area of 31.5 km2 in the Kongsfjord area close to the research station Ny-Ålesund (79° N 12°E) on the northwest coast of Spitsbergen. The basin is 54% glacier...

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