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Search: WFRF:(Stolte Jannes) > (2011-2014) > Quantifying the hyd...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00003955naa a2200541 4500
001oai:DiVA.org:su-101491
003SwePub
008140310s2014 | |||||||||||000 ||eng|
009oai:DiVA.org:vti-6636
009oai:DiVA.org:kth-140635
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1014912 URI
0247 a https://doi.org/10.1016/j.scitotenv.2013.07.0472 DOI
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:vti:diva-66362 URI
0247 a https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-1406352 URI
040 a (SwePub)sud (SwePub)vtid (SwePub)kth
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
1001 a Kalantari, Zahrau KTH,Mark- och vattenteknik4 aut0 (Swepub:kth)u1dxr4oj
2451 0a Quantifying the hydrological impact of simulated changes in land use on peak discharge in a small catchment
264 1b Elsevier BV,c 2014
338 a print2 rdacarrier
500 a AuthorCount:7;
500 a QC 20140130
520 a A physically-based, distributed hydrological model (MIKE SHE) was used to quantify overland runoff in response to four extreme rain events and four types of simulated land use measure in a catchment in Norway. The current land use in the catchment comprises arable lands, forest, urban areas and a stream that passes under a motorway at the catchment outlet. This model simulation study demonstrates how the composition and configuration of land use measures affect discharge at the catchment outlet differently in response to storms of different sizes. For example, clear-cutting on 30% of the catchment area produced a 60% increase in peak discharge and a 10% increase in total runoff resulting from a 50-year storm event in summer, but the effects on peak discharge were less pronounced during smaller storms. Reforestation of 60% of the catchment area was the most effective measure in reducing peak flows for smaller (2-, 5- and 10-year) storms. Introducing grassed waterways reduced water velocity in the stream and resulted in a 28% reduction in peak flow at the catchment outlet for the 50-year storm event. Overall, the results indicate that the specific effect of land use measures on catchment discharge depends on their spatial distribution and on the size and timing of storm events.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Miljövetenskap0 (SwePub)105022 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Environmental Sciences0 (SwePub)105022 hsv//eng
653 a Extreme rainfall-runoff events
653 a Road infrastructure
653 a Hydrological model
653 a Runoff
653 a Land use change
653 a U Science
7001 a Lyon, Steve W.u Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)4 aut0 (Swepub:su)stlyo
7001 a Folkeson, Lennart,d 1950-u KTH,Mark- och vattenteknik4 aut0 (Swepub:kth)u1id2cg0
7001 a French, Helen K.u Norwegian University of Life Sciences4 aut
7001 a Stolte, Jannesu Norwegian Institute for Agricultural and Environmental Research4 aut
7001 a Jansson, Per-Eriku KTH,Mark- och vattenteknik4 aut0 (Swepub:kth)u1rtodsk
7001 a Sassner, Monau DHI Sverige AB4 aut
7102 a KTHb Mark- och vattenteknik4 org
7730 t Science of the Total Environmentd : Elsevier BVg 466, s. 741-754q 466<741-754x 0048-9697x 1879-1026
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-101491
8564 8u https://doi.org/10.1016/j.scitotenv.2013.07.047
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:vti:diva-6636
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-140635

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