File Download
  Links for fulltext
     (May Require Subscription)
Supplementary

Article: Modeling boreal forest evapotranspiration and water balance at stand and catchment scales: a spatial approach

TitleModeling boreal forest evapotranspiration and water balance at stand and catchment scales: a spatial approach
Authors
Issue Date2019
PublisherCopernicus GmbH. The Journal's web site is located at http://www.copernicus.org/EGU/hess/hess.html
Citation
Hydrology and Earth System Sciences, 2019, v. 23, p. 3457-3480 How to Cite?
AbstractVegetation is known to have strong influence onevapotranspiration (ET), a major component of terrestrialwater balance. Yet hydrological models often describe ETby methods unable to include the variability of vegetationcharacteristics in their predictions. To take advantage of theincreasing availability of high-resolution open GIS data onland use, vegetation and soil characteristics in the borealzone, a modular, spatially distributed model for predictingET and other hydrological processes from grid cell to catch-ment level is presented and validated. An improved approachto upscale stomatal conductance to canopy scale using in-formation on plant type (conifer/deciduous) and stand leaf-area index (LAI) is proposed by coupling a common leaf-scale stomatal conductance model with a simple canopy radi-ation transfer scheme. Further, a generic parametrization forvegetation-related hydrological processes for Nordic borealforests is derived based on literature and data from a borealFluxNet site. With the generic parametrization, the modelwas shown to reproduce daily ET measured using an eddy-covariance technique well at 10 conifer-dominated Nordicforests whose LAI ranged from 0.2 to 6.8 m2m−2. Topogra-phy, soil and vegetation properties at 21 small boreal headwa-ter catchments in Finland were derived from open GIS dataat 16 m×16 m grid size to upscale water balance from standto catchment level. The predictions of annual ET and specificdischarge were successful in all catchments, located from 60to 68◦N, and daily discharge was also reasonably well pre-dicted by calibrating only one parameter against dischargemeasurements. The role of vegetation heterogeneity in soilmoisture and partitioning of ET was demonstrated. The pro-posed framework can support, for example, forest traffica-bility forecasting and predicting impacts of climate changeand forest management on stand and catchment water bal-ance. With appropriate parametrization it can be generalizedoutside the boreal coniferous forests.
Persistent Identifierhttp://hdl.handle.net/10722/272874
ISSN
2023 Impact Factor: 5.7
2023 SCImago Journal Rankings: 1.763
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorLauniainen, S-
dc.contributor.authorGuan, M-
dc.contributor.authorSalmivaara, A-
dc.contributor.authorKieloaho, AJ-
dc.date.accessioned2019-08-06T09:18:11Z-
dc.date.available2019-08-06T09:18:11Z-
dc.date.issued2019-
dc.identifier.citationHydrology and Earth System Sciences, 2019, v. 23, p. 3457-3480-
dc.identifier.issn1027-5606-
dc.identifier.urihttp://hdl.handle.net/10722/272874-
dc.description.abstractVegetation is known to have strong influence onevapotranspiration (ET), a major component of terrestrialwater balance. Yet hydrological models often describe ETby methods unable to include the variability of vegetationcharacteristics in their predictions. To take advantage of theincreasing availability of high-resolution open GIS data onland use, vegetation and soil characteristics in the borealzone, a modular, spatially distributed model for predictingET and other hydrological processes from grid cell to catch-ment level is presented and validated. An improved approachto upscale stomatal conductance to canopy scale using in-formation on plant type (conifer/deciduous) and stand leaf-area index (LAI) is proposed by coupling a common leaf-scale stomatal conductance model with a simple canopy radi-ation transfer scheme. Further, a generic parametrization forvegetation-related hydrological processes for Nordic borealforests is derived based on literature and data from a borealFluxNet site. With the generic parametrization, the modelwas shown to reproduce daily ET measured using an eddy-covariance technique well at 10 conifer-dominated Nordicforests whose LAI ranged from 0.2 to 6.8 m2m−2. Topogra-phy, soil and vegetation properties at 21 small boreal headwa-ter catchments in Finland were derived from open GIS dataat 16 m×16 m grid size to upscale water balance from standto catchment level. The predictions of annual ET and specificdischarge were successful in all catchments, located from 60to 68◦N, and daily discharge was also reasonably well pre-dicted by calibrating only one parameter against dischargemeasurements. The role of vegetation heterogeneity in soilmoisture and partitioning of ET was demonstrated. The pro-posed framework can support, for example, forest traffica-bility forecasting and predicting impacts of climate changeand forest management on stand and catchment water bal-ance. With appropriate parametrization it can be generalizedoutside the boreal coniferous forests.-
dc.languageeng-
dc.publisherCopernicus GmbH. The Journal's web site is located at http://www.copernicus.org/EGU/hess/hess.html-
dc.relation.ispartofHydrology and Earth System Sciences-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.titleModeling boreal forest evapotranspiration and water balance at stand and catchment scales: a spatial approach-
dc.typeArticle-
dc.identifier.emailGuan, M: mfguan@hku.hk-
dc.identifier.authorityGuan, M=rp02461-
dc.description.naturepublished_or_final_version-
dc.identifier.doi10.5194/hess-23-3457-2019-
dc.identifier.scopuseid_2-s2.0-85071445197-
dc.identifier.hkuros300263-
dc.identifier.volume23-
dc.identifier.spage3457-
dc.identifier.epage3480-
dc.identifier.isiWOS:000483023900001-
dc.publisher.placeGermany-
dc.identifier.issnl1027-5606-

Export via OAI-PMH Interface in XML Formats


OR


Export to Other Non-XML Formats