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  • 1.
    Brandt, Maja
    SMHI, Core Services.
    GENERATION, TRANSPORT AND DEPOSITION OF SUSPENDED AND DISSOLVED MATERIAL - EXAMPLES FROM SWEDISH RIVERS1990In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 72, no 3-4, p. 273-283Article in journal (Refereed)
    Abstract [en]

    Soil erosion, sediment transport and deposition in river systems in Sweden are discussed. The database consists of observations from a research project and from the Swedish network for the measurement of sediment transport. Examples are given from measurements in small plots, and from river basins of different sizes and characteristics. Effects of hydrological regime, of deposition in lakes, and of geology and human impact are illustrated. It was found that observations of erosion losses in index plots cannot easily be extrapolated to large areas, and that trends of transport most likely reflect trends in runoff.

  • 2.
    Nyberg, Alf
    SMHI.
    SOME VIEWS ON THE WATER LEVEL IN LAKE MALAREN AND IN THE ADJACENT BALTIC SEA1987In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 69, no 2, p. 271-282Article in journal (Refereed)
  • 3.
    Vedin, Haldo
    SMHI.
    FREQUENCY OF RARE WEATHER EVENTS DURING PERIODS OF EXTREME CLIMATE1990In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 72, no 2, p. 151-155Article in journal (Refereed)
  • 4.
    Vedin, Haldo
    et al.
    SMHI.
    Eklund, Anna
    SMHI, Core Services.
    Alexandersson, Hans
    SMHI.
    The rainstorm and flash flood at Mount Fulufjallet in August 1997: The meteorological and hydrological situation1999In: Geografiska Annaler. Series A, Physical Geography, ISSN 0435-3676, E-ISSN 1468-0459, Vol. 81A, no 3, p. 361-368Article in journal (Refereed)
    Abstract [en]

    The flood at Mount Fulufjallet, 30-31 August 1997 was caused by the most furious rainstorm ever documented in Sweden. Private measurements on the mountain show nor less than 276 mm over 24 hours, and the distribution of severe damage suggests even higher amounts in other parts of the mountain. The precipitation was connected to a front attacking a high pressure that had been dominating the weather in Sweden for several weeks, but orographic lifting on the east-facing slopes of the mountain may partly have caused the extreme intensity. In River Fulan. one of the upper branches of River Dalalven, the discharge peaked at a diurnal mean value of 233 m(3)/s, the highest since measurements began in 1913. At the stream Tangan and the new common outlet of the streams Store and Lilla Goljan, both locations with a normal discharge of only around 1 m(3)/s, instantaneous values of approximately 300 m(3)/s have been estimated, corresponding to values close to the normal discharge at the mouth of River Dalalven on the coast of the Sea of Bothnia.

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