Data

Boyagin FLUXNET Release 2025_r1

Terrestrial Ecosystem Research Network
Beringer, Jason
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.25901/etr2-2p40&rft.title=Boyagin FLUXNET Release 2025_r1&rft.identifier=10.25901/etr2-2p40&rft.publisher=Terrestrial Ecosystem Research Network&rft.description=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 (v3.4.21) 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 Boyagin Wandoo Woodland flux station is located approximately 12km west of Pingelly, near Perth, Western Australia. It was established in September 2017 and is managed by the University of Western Australia. The flux tower site is located within an area of wandoo woodland. The surrounding area is dominated by broadacre farming practices. Elevation of the site is close to 484m and mean annual precipitation at a nearby Bureau of Meteorology site at Pingelly measures 446mm. Maximum temperatures range from 15.3°C (in July) to 31.9°C (in Jan), while minimum temperatures range from 5.5°C (in July) to 15.5°C (in Jan). The instrument mast is 4 meters tall. Heat, water vapour, and carbon dioxide measurements are taken using the open-path eddy flux technique. Temperature, humidity, wind speed, wind direction, rainfall and net radiation are measured. Soil heat fluxes are measured and soil moisture content are collected.Data collected using standard eddy covariance and meteorological instrumentation on a 4m tower at the Boyagin 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.Data CreationData is measured using standard micro-meteorological instrumentation on a flux tower.Data is recorded on a data logger and is collected by the site PI.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.Filtering for low-ustar conditions, gap filling and partitioning of NEE into GPP and ER are done using ONEFlux.Progress Code: completedMaintenance and Update Frequency: annually&rft.creator=Beringer, Jason &rft.date=2026&rft.edition=2025_r1&rft.coverage=The Boyagin Wandoo Woodland flux tower is located in the wheatbelt of Western Australia about 200km southeast from Perth, Western Australia.&rft.coverage=northlimit=-32.43; southlimit=-32.53; westlimit=116.89; eastLimit=116.99; projection=EPSG:4326&rft_rights=Creative Commons Attribution 4.0 International Licence http://creativecommons.org/licenses/by/4.0&rft_rights=TERN services are provided on an as-is and as available basis. Users use any TERN services at their discretion and risk. They will be solely responsible for any damage or loss whatsoever that results from such use including use of any data obtained through TERN and any analysis performed using the TERN infrastructure. <br />Web links to and from external, third party websites should not be construed as implying any relationships with and/or endorsement of the external site or its content by TERN. <br /><br />Please advise any work or publications that use this data via the online form at https://www.tern.org.au/research-publications/#reporting&rft_rights=Please cite this dataset as {Author} ({PublicationYear}). {Title}. {Version, as appropriate}. Terrestrial Ecosystem Research Network. Dataset. {Identifier}.&rft_subject=climatologyMeteorologyAtmosphere&rft_subject=environment&rft_subject=NET ECOSYSTEM CO2 EXCHANGE (NEE)&rft_subject=GROSS PRIMARY PRODUCTION (GPP)&rft_subject=RESPIRATION RATE&rft_subject=EARTH SCIENCE&rft_subject=BIOSPHERE&rft_subject=ECOLOGICAL DYNAMICS&rft_subject=ECOSYSTEM FUNCTIONS&rft_subject=VERTICAL WIND VELOCITY/SPEED&rft_subject=WATER VAPOR PROCESSES&rft_subject=CARBON FLUX&rft_subject=EVAPOTRANSPIRATION&rft_subject=ATMOSPHERE&rft_subject=ATMOSPHERIC WATER VAPOR&rft_subject=SOILS&rft_subject=SENSIBLE HEAT FLUX&rft_subject=WATER VAPOR&rft_subject=LATENT HEAT FLUX&rft_subject=LONGWAVE RADIATION&rft_subject=WIND DIRECTION PROFILES&rft_subject=SHORTWAVE RADIATION&rft_subject=RAIN&rft_subject=PRECIPITATION&rft_subject=LIQUID PRECIPITATION&rft_subject=AIR TEMPERATURE&rft_subject=ATMOSPHERIC TEMPERATURE&rft_subject=SURFACE TEMPERATURE&rft_subject=HUMIDITY&rft_subject=Carbon Sequestration Science&rft_subject=ENVIRONMENTAL SCIENCES&rft_subject=SOIL SCIENCES&rft_subject=Ecosystem Function&rft_subject=ECOLOGICAL APPLICATIONS&rft_subject=ATMOSPHERIC SCIENCES&rft_subject=EARTH SCIENCES&rft_subject=Climatology&rft_subject=Meteorology&rft_subject=Climate change impacts and adaptation&rft_subject=net primary productivity of biomass expressed as carbon accumulated in miscellaneous living matter (Micromole per Square Metre Second)&rft_subject=Micromole per Square Metre Second&rft_subject=air temperature (Degree Celsius)&rft_subject=Degree Celsius&rft_subject=downward heat flux at ground level in soil (Watt Square Metre)&rft_subject=Watt Square Metre&rft_subject=ecosystem respiration (Micromole per Square Metre Square Second)&rft_subject=Micromole per Square Metre Square Second&rft_subject=gross primary productivity (Micromole per Square Metre Square Second)&rft_subject=lateral component of wind speed (Metre per Second)&rft_subject=Metre per Second&rft_subject=longitudinal component of wind speed (Metre per Second)&rft_subject=magnitude of surface downward stress (Kilograms per metre per square second)&rft_subject=Kilograms per metre per square second&rft_subject=mass concentration of water vapor in air (Gram per Cubic Metre)&rft_subject=Gram per Cubic Metre&rft_subject=mole fraction of carbon monoxide in dry air (Micromole per Mole)&rft_subject=Micromole per Mole&rft_subject=mole fraction of water vapor in air (Millimole per Mole)&rft_subject=Millimole per Mole&rft_subject=Monin-Obukhov length (Metre)&rft_subject=Metre&rft_subject=net ecosystem exchange (Micromole per Square Metre Second)&rft_subject=net ecosystem productivity (Micromole per Square Metre Second)&rft_subject=relative humidity (Percent)&rft_subject=Percent&rft_subject=soil temperature (Degree Celsius)&rft_subject=surface air pressure (Kilopascal)&rft_subject=Kilopascal&rft_subject=surface downwelling longwave flux in air (Watt per Square Metre)&rft_subject=Watt per Square Metre&rft_subject=surface downwelling shortwave flux in air (Watt per Square Metre)&rft_subject=surface friction velocity (Metre per Second)&rft_subject=surface net downward radiative flux (Watt per Square Metre)&rft_subject=surface upward latent heat flux (Watt per Square Metre)&rft_subject=surface upward mole flux of carbon dioxide (Micromole per Square Metre Second)&rft_subject=surface upward sensible heat flux (Watt per Square Metre)&rft_subject=surface upwelling longwave flux in air (Watt per Square Metre)&rft_subject=surface upwelling shortwave flux in air (Watt per Square Metre)&rft_subject=thickness of rainfall amount (Millimetre)&rft_subject=Millimetre&rft_subject=volume fraction of condensed water in soil (Cubic Metre per Cubic Metre)&rft_subject=Cubic Metre per Cubic Metre&rft_subject=wind from direction (Degree)&rft_subject=Degree&rft_subject=wind speed (Metre per Second)&rft_subject=250 meters - < 500 meters&rft_subject=1 minute - < 1 hour&rft_subject=AU-Boy&rft_subject=FLUXNET ID&rft.type=dataset&rft.language=English Access the data

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TERN services are provided on an "as-is" and "as available" basis. Users use any TERN services at their discretion and risk. They will be solely responsible for any damage or loss whatsoever that results from such use including use of any data obtained through TERN and any analysis performed using the TERN infrastructure.
Web links to and from external, third party websites should not be construed as implying any relationships with and/or endorsement of the external site or its content by TERN.

Please advise any work or publications that use this data via the online form at https://www.tern.org.au/research-publications/#reporting

Please cite this dataset as {Author} ({PublicationYear}). {Title}. {Version, as appropriate}. Terrestrial Ecosystem Research Network. Dataset. {Identifier}.

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Contact Information

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Building 1019, 80 Meiers Rd
QLD 4068
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Brief description


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 (v3.4.21) 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 Boyagin Wandoo Woodland flux station is located approximately 12km west of Pingelly, near Perth, Western Australia. It was established in September 2017 and is managed by the University of Western Australia. The flux tower site is located within an area of wandoo woodland. The surrounding area is dominated by broadacre farming practices. Elevation of the site is close to 484m and mean annual precipitation at a nearby Bureau of Meteorology site at Pingelly measures 446mm. Maximum temperatures range from 15.3°C (in July) to 31.9°C (in Jan), while minimum temperatures range from 5.5°C (in July) to 15.5°C (in Jan). The instrument mast is 4 meters tall. Heat, water vapour, and carbon dioxide measurements are taken using the open-path eddy flux technique. Temperature, humidity, wind speed, wind direction, rainfall and net radiation are measured. Soil heat fluxes are measured and soil moisture content are collected.

Lineage

Data collected using standard eddy covariance and meteorological instrumentation on a 4m tower at the Boyagin 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.

Data Creation
Data is measured using standard micro-meteorological instrumentation on a flux tower.
Data is recorded on a data logger and is collected by the site PI.
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.
Filtering for low-ustar conditions, gap filling and partitioning of NEE into GPP and ER are done using ONEFlux.

Progress Code: completed
Maintenance and Update Frequency: annually

Notes

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 Boyagin flux station is to:
  • -Monitor and determine the balance of environmental demands for water yields, agricultural productivity, GHG budgets and biodiversity within a catchment landscape.
  • -Provide information to establish a modelling tool for GHG and water fluxes across various land use types, in order to benefit land management practices in the wheatbelt of Western Australia.
The tower is a crucial component of the UWA critical zone observatory which will be the site of a multidisciplinary approach to understanding the landscape dynamics.
Data Quality Information

Data Quality Assessment Scope
local : dataset
The data have been quality controlled using the PyFluxPro software. Quality control checks applied to the data include:<ul style="list-style-type: disc;"> <li>range checks for plausible limits</li> <li>spike detection and removal</li> <li>dependency on other variables</li> <li>manual rejection of date ranges</li></ul> <br> 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.</br> <br>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. </br> <br>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.</br>

Isaac P., Cleverly J., McHugh I., van Gorsel E., Ewenz C. and Beringer, J. (2017). OzFlux data: network integration from collection to curation, Biogeosciences, 14: 2903-2928
doi : https://doi.org/10.5194/bg-14-2903-2017

Data Quality Assessment Result
local : Quality Result
No anomalous data detected after quality control.

Created: 2025-12-11

Issued: 2026-03-25

Modified: 2026-03-25

Data time period: 2017-10-20 to 2025-01-01

This dataset is part of a larger collection

Click to explore relationships graph

116.99,-32.43 116.99,-32.53 116.89,-32.53 116.89,-32.43 116.99,-32.43

116.94,-32.48

text: The Boyagin Wandoo Woodland flux tower is located in the wheatbelt of Western Australia about 200km southeast from Perth, Western Australia.

Subjects
1 minute - < 1 hour | 250 meters - < 500 meters | AIR TEMPERATURE | ATMOSPHERE | Atmospheric Sciences | ATMOSPHERIC TEMPERATURE | ATMOSPHERIC WATER VAPOR | AU-Boy | BIOSPHERE | CARBON FLUX | Carbon Sequestration Science | Climate change impacts and adaptation | Climatology | Cubic Metre per Cubic Metre | Degree | Degree Celsius | EARTH SCIENCE | Earth Sciences | Ecological Applications | ECOLOGICAL DYNAMICS | ECOSYSTEM FUNCTIONS | Environmental Sciences | EVAPOTRANSPIRATION | Ecosystem Function | FLUXNET ID | GROSS PRIMARY PRODUCTION (GPP) | Gram per Cubic Metre | HUMIDITY | Kilograms per metre per square second | Kilopascal | LATENT HEAT FLUX | LIQUID PRECIPITATION | LONGWAVE RADIATION | Meteorology | Metre | Metre per Second | Micromole per Mole | Micromole per Square Metre Second | Micromole per Square Metre Square Second | Millimetre | Millimole per Mole | Monin-Obukhov length (Metre) | NET ECOSYSTEM CO2 EXCHANGE (NEE) | PRECIPITATION | Percent | RAIN | RESPIRATION RATE | SENSIBLE HEAT FLUX | SHORTWAVE RADIATION | Soil Sciences | SOILS | SURFACE TEMPERATURE | VERTICAL WIND VELOCITY/SPEED | WATER VAPOR | WATER VAPOR PROCESSES | WIND DIRECTION PROFILES | Watt Square Metre | Watt per Square Metre | air temperature (Degree Celsius) | climatologyMeteorologyAtmosphere | downward heat flux at ground level in soil (Watt Square Metre) | ecosystem respiration (Micromole per Square Metre Square Second) | environment | gross primary productivity (Micromole per Square Metre Square Second) | lateral component of wind speed (Metre per Second) | longitudinal component of wind speed (Metre per Second) | magnitude of surface downward stress (Kilograms per metre per square second) | mass concentration of water vapor in air (Gram per Cubic Metre) | mole fraction of carbon monoxide in dry air (Micromole per Mole) | mole fraction of water vapor in air (Millimole per Mole) | net ecosystem exchange (Micromole per Square Metre Second) | net ecosystem productivity (Micromole per Square Metre Second) | net primary productivity of biomass expressed as carbon accumulated in miscellaneous living matter (Micromole per Square Metre Second) | relative humidity (Percent) | soil temperature (Degree Celsius) | surface air pressure (Kilopascal) | surface downwelling longwave flux in air (Watt per Square Metre) | surface downwelling shortwave flux in air (Watt per Square Metre) | surface friction velocity (Metre per Second) | surface net downward radiative flux (Watt per Square Metre) | surface upward latent heat flux (Watt per Square Metre) | surface upward mole flux of carbon dioxide (Micromole per Square Metre Second) | surface upward sensible heat flux (Watt per Square Metre) | surface upwelling longwave flux in air (Watt per Square Metre) | surface upwelling shortwave flux in air (Watt per Square Metre) | thickness of rainfall amount (Millimetre) | volume fraction of condensed water in soil (Cubic Metre per Cubic Metre) | wind from direction (Degree) | wind speed (Metre per Second) |

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Other Information
Point-of-truth metadata URL

uri : https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/eb507963-a476-4837-b948-f5a0b773c2d6

Isaac P., Cleverly J., McHugh I., van Gorsel E., Ewenz C. and Beringer, J. (2017). OzFlux data: network integration from collection to curation, Biogeosciences, 14: 2903-2928

doi : https://doi.org/10.5194/bg-14-2903-2017

PyFluxPro

uri : https://github.com/OzFlux/PyFluxPro

ONEFlux

uri : https://github.com/fluxnet/ONEFlux

Pastorello, G., Trotta, C., Canfora, E. et al. The FLUXNET2015 dataset and the ONEFlux processing pipeline for eddy covariance data. Sci Data 7, 225 (2020).

doi : https://doi.org/10.1038/s41597-020-0534-3