The role of catchment scale and landscape characteristics for runoff generation of boreal streams

The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal streams within the Krycklan catchment in northern Sweden. We used detailed oxygen-18 analyses of soils from two characteristic landscape types, sno...

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Veröffentlicht in:	Journal of hydrology (Amsterdam) Jg. 344; H. 3; S. 198 - 209
Hauptverfasser:	Laudon, Hjalmar, Sjöblom, Viktor, Buffam, Ishi, Seibert, Jan, Mörth, Magnus
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Amsterdam Elsevier B.V 15.10.2007 Elsevier Science
Schlagworte:	Boreal boreal streams Earth sciences Earth, ocean, space Exact sciences and technology forested watersheds Geochemistry Hydrograph separation Hydrology Hydrology. Hydrogeology Isotope geochemistry Isotope geochemistry. Geochronology Landscape characteristics landscapes Mineralogy Oxygen-18 runoff Scale Silicates Snow melt snowmelt stream flow streams Sweden Water geochemistry watershed hydrology watersheds wetlands Sweden Scandinavia Landscape characteristics Scale Boreal Oxygen-18 Snow melt Hydrograph separation landscapes floods stable isotopes O-18/O-16 Europe streams runoff forests meltwater drainage basins wetlands hydrochemistry snow boreal zone soils hydrographs
ISSN:	0022-1694, 1879-2707
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Abstract	The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal streams within the Krycklan catchment in northern Sweden. We used detailed oxygen-18 analyses of soils from two characteristic landscape types, snow melt samples and water samples from 15 streams with subcatchments ranging in size from 0.03 to 67 km 2. The detailed process understanding that was derived from isotopic and hydrometric measurements at a wetland and a forest site, in combination with the stream monitoring, enabled the development of a conceptual framework that could explain the variability in hydrological pathways over a range of catchment scales. While the proportion of new or event water was over 50% in wetland dominated catchments, the event water contribution in forested catchments was between 10% and 30%. The results suggest a large degree of scale-independence of hydrological flow pathways during the snow melt period, controlled by the proportion of wetland and median subcatchment area, across three orders of magnitude in spatial scale. The results from this study highlighted the importance of different runoff generation processes in different landscape elements, an understanding that can be useful in disentangling the temporal dynamics in hydrology and biogeochemistry during snow melt episodes when moving from small headwater streams to catchment outlets.
AbstractList	The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal streams within the Krycklan catchment in northern Sweden. We used detailed oxygen-18 analyses of soils from two characteristic landscape types, snow melt samples and water samples from 15 streams with subcatchments ranging in size from 0.03 to 67 km2. The detailed process understanding that was derived from isotopic and hydrometric measurements at a wetland and a forest site, in combination with the stream monitoring, enabled the development of a conceptual framework that could explain the variability in hydrological pathways over a range of catchment scales. While the proportion of new or event water was over 50% in wetland dominated catchments, the event water contribution in forested catchments was between 10% and 30%. The results suggest a large degree of scale-independence of hydrological flow pathways during the snow melt period, controlled by the proportion of wetland and median subcatchment area, across three orders of magnitude in spatial scale. The results from this study highlighted the importance of different runoff generation processes in different landscape elements, an understanding that can be useful in disentangling the temporal dynamics in hydrology and biogeochemistry during snow melt episodes when moving from small headwater streams to catchment outlets. The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal streams within the Krycklan catchment in northern Sweden. We used detailed oxygen-18 analyses of soils from two characteristic landscape types, snow melt samples and water samples from 15 streams with subcatchments ranging in size from 0.03 to 67km super(2). The detailed process understanding that was derived from isotopic and hydrometric measurements at a wetland and a forest site, in combination with the stream monitoring, enabled the development of a conceptual framework that could explain the variability in hydrological pathways over a range of catchment scales. While the proportion of new or event water was over 50% in wetland dominated catchments, the event water contribution in forested catchments was between 10% and 30%. The results suggest a large degree of scale-independence of hydrological flow pathways during the snow melt period, controlled by the proportion of wetland and median subcatchment area, across three orders of magnitude in spatial scale. The results from this study highlighted the importance of different runoff generation processes in different landscape elements, an understanding that can be useful in disentangling the temporal dynamics in hydrology and biogeochemistry during snow melt episodes when moving from small headwater streams to catchment outlets. The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal streams within the Krycklan catchment in northern Sweden. We used detailed oxygen-18 analyses of soils from two characteristic landscape types, snow melt samples and water samples from 15 streams with subcatchments ranging in size from 0.03 to 67 km 2. The detailed process understanding that was derived from isotopic and hydrometric measurements at a wetland and a forest site, in combination with the stream monitoring, enabled the development of a conceptual framework that could explain the variability in hydrological pathways over a range of catchment scales. While the proportion of new or event water was over 50% in wetland dominated catchments, the event water contribution in forested catchments was between 10% and 30%. The results suggest a large degree of scale-independence of hydrological flow pathways during the snow melt period, controlled by the proportion of wetland and median subcatchment area, across three orders of magnitude in spatial scale. The results from this study highlighted the importance of different runoff generation processes in different landscape elements, an understanding that can be useful in disentangling the temporal dynamics in hydrology and biogeochemistry during snow melt episodes when moving from small headwater streams to catchment outlets.
Author	Seibert, Jan Laudon, Hjalmar Buffam, Ishi Mörth, Magnus Sjöblom, Viktor
Author_xml	– sequence: 1 givenname: Hjalmar surname: Laudon fullname: Laudon, Hjalmar email: hjalmar.laudon@emg.umu.se organization: Ecology and Environmental Science, Umeå University, 901 87 Umeå, Sweden – sequence: 2 givenname: Viktor surname: Sjöblom fullname: Sjöblom, Viktor organization: Ecology and Environmental Science, Umeå University, 901 87 Umeå, Sweden – sequence: 3 givenname: Ishi surname: Buffam fullname: Buffam, Ishi organization: Department of Forest Ecology, Swedish University of Agricultural Sciences, 901 83 Umeå, Sweden – sequence: 4 givenname: Jan surname: Seibert fullname: Seibert, Jan organization: Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden – sequence: 5 givenname: Magnus surname: Mörth fullname: Mörth, Magnus organization: Department of Geology and Geochemistry, Stockholm University, S-106 91 Stockholm, Sweden
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Snippet	The effect of catchment scale and the influence of landscape characteristics on runoff generation were investigated during snow melt in 15 nested boreal...
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SubjectTerms	Boreal boreal streams Earth sciences Earth, ocean, space Exact sciences and technology forested watersheds Geochemistry Hydrograph separation Hydrology Hydrology. Hydrogeology Isotope geochemistry Isotope geochemistry. Geochronology Landscape characteristics landscapes Mineralogy Oxygen-18 runoff Scale Silicates Snow melt snowmelt stream flow streams Sweden Water geochemistry watershed hydrology watersheds wetlands
Title	The role of catchment scale and landscape characteristics for runoff generation of boreal streams
URI	https://dx.doi.org/10.1016/j.jhydrol.2007.07.010 https://www.proquest.com/docview/21011529 https://www.proquest.com/docview/48117640
Volume	344
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