Urban snowmelt and runoff in northern Sweden

Snowmelt and runoff in urban areas in Lulea, north Sweden, are discussed and compared with rural conditions. The uneven snow distribution in cities is quantified. Energy fluxes at the snow surface in different environments are estimated. It is shown that, mainly because of increased absorbed radiati...

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Bibliographic Details
Main Authors: Bengtsson, Lars, Westerstrom, G.
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis 1992
Subjects:
Online Access:https://lup.lub.lu.se/record/2595281
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author Bengtsson, Lars
Westerstrom, G.
author_facet Bengtsson, Lars
Westerstrom, G.
author_sort Bengtsson, Lars
collection Lund University Publications (LUP)
description Snowmelt and runoff in urban areas in Lulea, north Sweden, are discussed and compared with rural conditions. The uneven snow distribution in cities is quantified. Energy fluxes at the snow surface in different environments are estimated. It is shown that, mainly because of increased absorbed radiative energy in the snow, the daily melt is about 10 mm higher in the city than in rural environments. In the course of prolonged snowmelt, the infiltration capacity of most soils in urban areas becomes so reduced that melt-induced peak flows from grassed and gravelled surfaces are similar to those from asphalted surfaces. When rain falls on snow, overland flow may take place from the entire area of a basin.
format Article in Journal/Newspaper
genre North Sweden
Northern Sweden
genre_facet North Sweden
Northern Sweden
geographic Lulea
geographic_facet Lulea
id ftulundlup:oai:lup.lub.lu.se:096ca1cd-1e47-4b11-9244-67b63ad61e35
institution Open Polar
language English
long_lat ENVELOPE(22.166,22.166,65.580,65.580)
op_collection_id ftulundlup
op_relation https://lup.lub.lu.se/record/2595281
scopus:0026453208
op_source Hydrological Sciences Journal; 37(3), pp 263-275 (1992)
ISSN: 0262-6667
publishDate 1992
publisher Taylor & Francis
record_format openpolar
spelling ftulundlup:oai:lup.lub.lu.se:096ca1cd-1e47-4b11-9244-67b63ad61e35 2025-04-06T15:01:17+00:00 Urban snowmelt and runoff in northern Sweden Bengtsson, Lars Westerstrom, G. 1992 https://lup.lub.lu.se/record/2595281 eng eng Taylor & Francis https://lup.lub.lu.se/record/2595281 scopus:0026453208 Hydrological Sciences Journal; 37(3), pp 263-275 (1992) ISSN: 0262-6667 Water Engineering contributiontojournal/article info:eu-repo/semantics/article text 1992 ftulundlup 2025-03-11T14:07:58Z Snowmelt and runoff in urban areas in Lulea, north Sweden, are discussed and compared with rural conditions. The uneven snow distribution in cities is quantified. Energy fluxes at the snow surface in different environments are estimated. It is shown that, mainly because of increased absorbed radiative energy in the snow, the daily melt is about 10 mm higher in the city than in rural environments. In the course of prolonged snowmelt, the infiltration capacity of most soils in urban areas becomes so reduced that melt-induced peak flows from grassed and gravelled surfaces are similar to those from asphalted surfaces. When rain falls on snow, overland flow may take place from the entire area of a basin. Article in Journal/Newspaper North Sweden Northern Sweden Lund University Publications (LUP) Lulea ENVELOPE(22.166,22.166,65.580,65.580)
spellingShingle Water Engineering
Bengtsson, Lars
Westerstrom, G.
Urban snowmelt and runoff in northern Sweden
title Urban snowmelt and runoff in northern Sweden
title_full Urban snowmelt and runoff in northern Sweden
title_fullStr Urban snowmelt and runoff in northern Sweden
title_full_unstemmed Urban snowmelt and runoff in northern Sweden
title_short Urban snowmelt and runoff in northern Sweden
title_sort urban snowmelt and runoff in northern sweden
topic Water Engineering
topic_facet Water Engineering
url https://lup.lub.lu.se/record/2595281