Hovenden, M. & Yates, B. (2026). Wedgetail FLUXNET Release 2026_r1. Version 2026_r1. Terrestrial Ecosystem Research Network. Dataset. https://dx.doi.org/10.25901/71r0-0836
Wedgetail FLUXNET Release 2026_r1
Ver: 2026_r1
Status of Data: completed
Update Frequency: annually
Security Classification: unclassified
Record Last Modified: 2026-04-02
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Dataset Created: 2026-03-19
Dataset Published: 2026-04-02
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This release consists of flux tower measurements of the exchange of energy and mass between the surface and the atmospheric boundary-layer using eddy covariance techniques. Data were processed using PyFluxPro as described by Isaac et al. (2017) for the quality control and post-processing steps. The final, gap-filled product containing Net Ecosystem Exchange (NEE) partitioned into Gross Primary Productivity (GPP) and Ecosystem Respiration (ER) has been produced using the ONEFlux software as described in Pastorello et al. (2020). This data set has been produced as part of the FLUXNET Shuttle project. The Wedge Tail flux tower (42°05'29"S, 147°04'46"E) is located on the traditional lands of the Lairmairrener people within the Silver Plains Reserve, a property managed by the Tasmanian Land Conservancy.
Installed on 29 July 2024 by the University of Tasmania, the Wedge Tail flux tower is situated approximately 550 meters from the adjacent Silver Plains Flux Tower.
The surrounding landscape is a gently south-southwest sloping, species-rich sedgeland and grassland, with a history of grazing. Positioned at an elevation of 860 meters, the site receives an average annual precipitation of approximately 900 mm. The soil at the site is organosol on a Jurassic dolerite geology. Average seasonal temperatures range from 16°C in summer to 6°C in winter.
Installed on 29 July 2024 by the University of Tasmania, the Wedge Tail flux tower is situated approximately 550 meters from the adjacent Silver Plains Flux Tower.
The surrounding landscape is a gently south-southwest sloping, species-rich sedgeland and grassland, with a history of grazing. Positioned at an elevation of 860 meters, the site receives an average annual precipitation of approximately 900 mm. The soil at the site is organosol on a Jurassic dolerite geology. Average seasonal temperatures range from 16°C in summer to 6°C in winter.
Credit
We at TERN acknowledge the Traditional Owners and Custodians throughout Australia, New Zealand and all nations. We honour their profound connections to land, water, biodiversity and culture and pay our respects to their Elders past, present and emerging.
Purpose
The purpose of the Wedgetail flux tower is to: - Monitor exchanges of carbon dioxide, water vapour and energy in a high-altitude grassy peatland ecosystem on the Tasmanian Central Plateau.
- Quantify the carbon balance of the ecosystem, along with the key components of net ecosystem exchange, gross primary productivity and ecosystem respiration.
- Identify key environmental and climatic drivers of carbon, water and energy fluxes.
- Complement manual chamber measurements of net ecosystem CO2 exchange in an adjacent climate change experiment.
- Utilize measurements alongside manual chamber measurements and ancillary environmental variables to model ecosystem carbon dynamics under a future climate. Furthermore Wedgetail serves as a control site for the Silver Plains flux tower (AU-Sil), situated ~550m east of Wedgetail, which will undergo hydrological remediation from 2027-2028.
- Quantify the carbon balance of the ecosystem, along with the key components of net ecosystem exchange, gross primary productivity and ecosystem respiration.
- Identify key environmental and climatic drivers of carbon, water and energy fluxes.
- Complement manual chamber measurements of net ecosystem CO2 exchange in an adjacent climate change experiment.
- Utilize measurements alongside manual chamber measurements and ancillary environmental variables to model ecosystem carbon dynamics under a future climate. Furthermore Wedgetail serves as a control site for the Silver Plains flux tower (AU-Sil), situated ~550m east of Wedgetail, which will undergo hydrological remediation from 2027-2028.
Lineage
Data collected using standard eddy covariance and meteorological instrumentation on a 2.6m tower at the Wedgetail site. The data were quality controlled using the PyFluxPro software package, see Isaac et al. (2017), which is available at https://github.com/OzFlux/PyFluxPro. Gap filling and partitioning has been done using the ONEFlux software package, see Pastorello et al. 2020, which is available at https://github.com/fluxnet/ONEFlux.
Method DocumentationPastorello, G., Trotta, C., Canfora, E. et al. The FLUXNET2015 dataset and the ONEFlux processing pipeline for eddy covariance data. Sci Data 7, 225 (2020).Isaac P., Cleverly J., McHugh I., van Gorsel E., Ewenz C. and Beringer, J. (2017). OzFlux data: network integration from collection to curation,PyFluxProONEFlux
Procedure Steps
1.
Data is measured using standard micro-meteorological instrumentation on a flux tower.
2.
Data is recorded on a data logger and is collected by the site PI.
3.
Data quality control including removal of data outside plausible ranges, removal of spikes, exclusion of particular date ranges and removal of data based on the dependence of one variable on another is done using PyFluxPro.
4.
Filtering for low-ustar conditions, gap filling and partitioning of NEE into GPP and ER are done using ONEFlux.
Spatial Description
The Wedge Tail flux tower is situated approximately 550 meters from the adjacent Silver Plains Flux Tower.
Temporal Coverage
From 2024-01-01 to 2025-08-25
Spatial Resolution
Data not provided.
Vertical Extent
Data not provided.
Data Quality Assessment Scope
Isaac P., Cleverly J., McHugh I., van Gorsel E., Ewenz C. and Beringer, J. (2017). OzThe data have been quality controlled using the PyFluxPro software. Quality control checks applied to the data include:
Specific checks applied to the sonic and IRGA data including rejection of points based on the sonic and IRGA diagnostic values and on either automatic gain control (AGC) or CO2 and H2O signal strength, depending upon the configuration of the IRGA.
If the data quality is poor, the meteorological data is filled from ERA5 reanalysis data and fluxes are filled using the Marginal Distribution Sampling method. Filled data can be identified by the Quality Controls flags in the dataset.
The ONEFlux software used to gap fill and partition this data set also applies a Median Absolute Deviation (MAD) filter to the carbon dioxide, latent heat and sensible heat before the gap filling step.
- range checks for plausible limits
- spike detection and removal
- dependency on other variables
- manual rejection of date ranges
Specific checks applied to the sonic and IRGA data including rejection of points based on the sonic and IRGA diagnostic values and on either automatic gain control (AGC) or CO2 and H2O signal strength, depending upon the configuration of the IRGA.
If the data quality is poor, the meteorological data is filled from ERA5 reanalysis data and fluxes are filled using the Marginal Distribution Sampling method. Filled data can be identified by the Quality Controls flags in the dataset.
The ONEFlux software used to gap fill and partition this data set also applies a Median Absolute Deviation (MAD) filter to the carbon dioxide, latent heat and sensible heat before the gap filling step.
Data Quality Assessment Outcome
No anomalous data detected after quality control.
ANZSRC - FOR
GCMD Sciences
Horizontal Resolution
Parameters
Platforms
Temporal Resolution
User Defined
AU-Wgt
FLUXNET ID
Author
Co-Author
Contact Point
Terrestrial Ecosystem Research Network
80 Meiers Road, Indooroopilly, Queensland, 4068, Australia.
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