https://ogma.newcastle.edu.au/vital/access/ /manager/Index en-au 5 https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:43289 Wed 24 May 2023 12:11:01 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:30844 Wed 24 May 2023 11:54:32 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:45920 Wed 22 Mar 2023 17:37:52 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3269 Wed 11 Apr 2018 13:20:21 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1368 Wed 11 Apr 2018 10:52:05 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:32627 Tue 26 Jun 2018 15:05:16 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:38449 Thu 26 May 2022 16:29:23 AEST ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:53387 Thu 23 Nov 2023 13:30:04 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:11162 Sat 24 Mar 2018 08:08:31 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:308 Sat 24 Mar 2018 07:42:23 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:22843 Eucalyptus regnans and E. delegatensis stands, correlated strongly with forest overstorey stocking density (R² 0.72). This curvilinear relationship was used with routine forest stocking density and basal area measurements to estimate sapwood area of the forest overstorey at various times in 15 research catchments in undisturbed and disturbed forests located in the Great Dividing Range, Victoria, Australia. Up to 45 years of annual precipitation and streamflow data available from the 15 catchments were used to examine relationships between mean annual loss (evapotranspiration estimated as mean annual precipitation minus mean annual streamflow), and sapwood area. Catchment mean sapwood area correlated strongly (R² 0.88) with catchment mean annual loss. Variation in sapwood area accounted for 68% more variation in mean annual streamflow than precipitation alone (R² 0.90 compared with R² 0.22). Changes in sapwood area accounted for 96% of the changes in mean annual loss observed after forest thinning or clear-cutting and regeneration. We conclude that forest inventory data can be used reliably to predict spatial and temporal variation in catchment annual losses and streamflow in response to natural and imposed disturbances in even-aged forests. Consequently, recent advances in mapping of sapwood area using airborne light detection and ranging will enable high resolution spatial and temporal mapping of mean annual loss and mean annual streamflow over large areas of forested catchment. This will be particularly beneficial in management of water resources from forested catchments subject to disturbance but lacking reliable long-term (years to decades) streamflow records.]]> Sat 24 Mar 2018 07:16:04 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:37721 Mon 14 Nov 2022 20:35:05 AEDT ]]> https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:42210 2 remote study area, a rainfall interpolation procedure using available rainfall data and information on terrain was integrated into a new seasonal streamflow model, called ABCF, which uses catchment sapwood area (SA) as the emergent property that equilibrates with potential evapotranspiration (PET), and a soil storage threshold that reduces AET below PET when soil water is limiting. We produce seasonal estimates of streamflow with Nash Sutcliffe efficiencies of 0.85, 0.87, and 0.91 for three major catchments within the study area. A fundamental feature of the "top-down" model approach is the use of LiDAR data and forest inventory data to model forest structural properties that relate strongly with SA. Building on our previous work with this modelling framework, our representation of eco-hydrological properties of the forest has been refined with a more accurate procedure for estimating stand mean sapwood thickness, and hence SA, and a remotely sensed tree stocking density (N) of old-growth forests to correct the temporal evolution of N as a means to improve SA estimates. Regional consistency of model parameters shows that the "top-down" modelling framework may be used to estimate streamflow in ungauged catchments using a forest growth model. The seasonal model generalised for both water-limited and water-unlimited forest conditions has significant potential for application in water supply planning and drought security.]]> Fri 26 Aug 2022 09:29:20 AEST ]]>