FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3142281376> ?p ?o ?g. }

• W3142281376 abstract "&lt;p&gt;The Australian Water Resources Assessment Landscape (AWRA-L) model is a continental gridded, daily time-step, water balance model, developed over the last decade by CSIRO and the Australian Bureau of Meteorology for a range of hydrological applications. The model outputs (including soil moisture, evapotranspiration, runoff and deep drainage; available through www.bom.gov.au/water/landscape) have found wide application for monitoring purposes (e.g. for flood and fire risk, drought monitoring), water reporting (eg. National Water Accounts), and in analysing trends in water balance outputs including streamflow. In addition to these historical/monitoring applications, AWRA-L is being further used for production of 10-day forecasts, seasonal forecasts, and long-term projections of hydrological outputs out to the end of the century.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;This study details recent development of AWRA-L for improved performance across the water balance for use in monitoring through to long term projections. Changes are implemented across three broad areas: improved static and dynamic inputs, altered conceptual structure (additional urban component and baseflow ephemerality), and altered calibration approach. In particular, a new spatial calibration approach is applied across the nation using over 300 catchments. To do so model pixel output values are compared against spatially distributed satellite data for soil moisture, evapotranspiration (ET), and two new components including fraction of vegetation (F&lt;sub&gt;veg&lt;/sub&gt;) and terrestrial water storage (TWS). In the previous versions of the model lumped catchment average values of evapotranspiration and soil moisture were used. In addition to comparing to a wide range of national datasets (streamflow observations, flux tower observations, soil moisture network observations, recharge observations), the model performance was compared for drought analysis (reproducing 2-state rainfall-runoff behaviour observed in parts of Australia) and flood analysis (correlating with operationally used flood forecasting parameters). Overall, the modified AWRA-L outperformed previous versions in terms of water balance estimation according to a wide range of validation data. The successful application of the spatial calibration method can potentially pave the path for more frequent application of complex calibration methods for large scale simulations. Furthermore, consideration of a terrestrial water storage component in the objective function highlights the importance of this factor in capturing more accurate simulation of other water balance components, particularly streamflow. The improved streamflow performance demonstrates the enhanced functionality of the model in capturing intermittency and streamflow shifts in seasonally dry and groundwater dependent catchments, further demonstrated in the drought analysis. Finally, the flood study demonstrates the application and value of the model for real time flood-monitoring and forecasting purposes. This study shows the potential of AWRA-L model and associated spatial calibration approach for accurate simulation of water balance variables for use in continental-scale studies.&lt;/p&gt;" @default.
• W3142281376 created "2021-04-13" @default.
• W3142281376 creator A5016219912 @default.
• W3142281376 creator A5026762896 @default.
• W3142281376 creator A5037205341 @default.
• W3142281376 creator A5047062560 @default.
• W3142281376 creator A5080802940 @default.
• W3142281376 date "2021-03-04" @default.
• W3142281376 modified "2023-10-14" @default.
• W3142281376 title "Recent improvements to the Australian Water Resources Assessment Landscape Model (version 7)" @default.
• W3142281376 doi "https://doi.org/10.5194/egusphere-egu21-15154" @default.
• W3142281376 hasPublicationYear "2021" @default.
• W3142281376 type Work @default.
• W3142281376 sameAs 3142281376 @default.
• W3142281376 citedByCount "1" @default.
• W3142281376 countsByYear W31422813762023 @default.
• W3142281376 crossrefType "posted-content" @default.
• W3142281376 hasAuthorship W3142281376A5016219912 @default.
• W3142281376 hasAuthorship W3142281376A5026762896 @default.
• W3142281376 hasAuthorship W3142281376A5037205341 @default.
• W3142281376 hasAuthorship W3142281376A5047062560 @default.
• W3142281376 hasAuthorship W3142281376A5080802940 @default.
• W3142281376 hasConcept C126197015 @default.
• W3142281376 hasConcept C126645576 @default.
• W3142281376 hasConcept C127313418 @default.
• W3142281376 hasConcept C127413603 @default.
• W3142281376 hasConcept C142724271 @default.
• W3142281376 hasConcept C153823671 @default.
• W3142281376 hasConcept C176783924 @default.
• W3142281376 hasConcept C187320778 @default.
• W3142281376 hasConcept C18903297 @default.
• W3142281376 hasConcept C205649164 @default.
• W3142281376 hasConcept C2776133958 @default.
• W3142281376 hasConcept C39432304 @default.
• W3142281376 hasConcept C49204034 @default.
• W3142281376 hasConcept C50477045 @default.
• W3142281376 hasConcept C53739315 @default.
• W3142281376 hasConcept C58640448 @default.
• W3142281376 hasConcept C66465714 @default.
• W3142281376 hasConcept C71924100 @default.
• W3142281376 hasConcept C76856003 @default.
• W3142281376 hasConcept C76886044 @default.
• W3142281376 hasConcept C86803240 @default.
• W3142281376 hasConceptScore W3142281376C126197015 @default.
• W3142281376 hasConceptScore W3142281376C126645576 @default.
• W3142281376 hasConceptScore W3142281376C127313418 @default.
• W3142281376 hasConceptScore W3142281376C127413603 @default.
• W3142281376 hasConceptScore W3142281376C142724271 @default.
• W3142281376 hasConceptScore W3142281376C153823671 @default.
• W3142281376 hasConceptScore W3142281376C176783924 @default.
• W3142281376 hasConceptScore W3142281376C187320778 @default.
• W3142281376 hasConceptScore W3142281376C18903297 @default.
• W3142281376 hasConceptScore W3142281376C205649164 @default.
• W3142281376 hasConceptScore W3142281376C2776133958 @default.
• W3142281376 hasConceptScore W3142281376C39432304 @default.
• W3142281376 hasConceptScore W3142281376C49204034 @default.
• W3142281376 hasConceptScore W3142281376C50477045 @default.
• W3142281376 hasConceptScore W3142281376C53739315 @default.
• W3142281376 hasConceptScore W3142281376C58640448 @default.
• W3142281376 hasConceptScore W3142281376C66465714 @default.
• W3142281376 hasConceptScore W3142281376C71924100 @default.
• W3142281376 hasConceptScore W3142281376C76856003 @default.
• W3142281376 hasConceptScore W3142281376C76886044 @default.
• W3142281376 hasConceptScore W3142281376C86803240 @default.
• W3142281376 hasLocation W31422813761 @default.
• W3142281376 hasOpenAccess W3142281376 @default.
• W3142281376 hasPrimaryLocation W31422813761 @default.
• W3142281376 hasRelatedWork W1977224 @default.
• W3142281376 hasRelatedWork W2052880 @default.
• W3142281376 hasRelatedWork W2505676 @default.
• W3142281376 hasRelatedWork W5501091 @default.
• W3142281376 hasRelatedWork W5733984 @default.
• W3142281376 hasRelatedWork W6022030 @default.
• W3142281376 hasRelatedWork W8434213 @default.
• W3142281376 hasRelatedWork W8611115 @default.
• W3142281376 hasRelatedWork W5973056 @default.
• W3142281376 hasRelatedWork W8305293 @default.
• W3142281376 isParatext "false" @default.
• W3142281376 isRetracted "false" @default.
• W3142281376 magId "3142281376" @default.
• W3142281376 workType "article" @default.