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Ash on snow a tool - a tool to prevent flooding?
Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, Geovetenskap och miljöteknik.
2001 (engelsk)Inngår i: Nordic Hydrology, ISSN 0029-1277, E-ISSN 1996-9694, Vol. 32, nr 3, s. 195-214Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Years with late spring in combination with thick snow-pack constitute risk for flooding. To decrease that risk, the possibility of spreading albedo-lowering material (wood ash) on parts of a basin snow has been examined. By blackening the snow more solar radiation is absorbed and the snowmelt is enhanced. If sun-exposed parts of the basin are ash-treated (before normal runoff starts) the runoff will be distributed over a longer period of time and the risk of flooding will be reduced. Wood ash in different concentrations was spread on small snow plots and melt rates and albedo were measured. For snow covered with 0.03 kg ash m super(-2), the albedo was decreased from approximately 0.60 for natural snow to approximately 0.25, resulting in approximately 90% more absorbed short-wave radiation. Melt on the ash treated surface, (daily average snow water equivalent), was 70% larger than melt on natural snow (12 and 7 mm d super(-1) respectively). A five times larger concentration (0.15 kg m super(-2)) only increased the melt rate to 14 mm d super(-1). The temperature-index method was shown to be inadequate for modelling the melt rate for the ash treated snow. A radiation-index model, based on absorbed incoming short wave radiation, was shown to model the melt rate better than the temperature-index method.

sted, utgiver, år, opplag, sider
2001. Vol. 32, nr 3, s. 195-214
HSV kategori
Forskningsprogram
Tillämpad geologi
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URN: urn:nbn:se:ltu:diva-11337Lokal ID: a4842e70-798c-11db-8824-000ea68e967bOAI: oai:DiVA.org:ltu-11337DiVA, id: diva2:984287
Merknad
Validerad; 2001; Bibliografisk uppgift: NORDIC Hydrological Conference 2000, Uppsala (Sweden), Jun 2000; 20061121 (ysko)Tilgjengelig fra: 2016-09-29 Laget: 2016-09-29 Sist oppdatert: 2017-11-24bibliografisk kontrollert

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