Data

Great Western Woodlands Flux Data Release 2022_v1

Terrestrial Ecosystem Research Network
Macfarlane, Craig ; Prober, Suzanne ; Wiehl, Georg
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.25901/z0d0-x433&rft.title=Great Western Woodlands Flux Data Release 2022_v1&rft.identifier=10.25901/z0d0-x433&rft.publisher=Terrestrial Ecosystem Research Network&rft.description=This data release consists of flux tower measurements of the exchange of energy and mass between the surface and the atmospheric boundary-layer in semi-arid eucalypt woodland using eddy covariance techniques. It been processed using PyFluxPro (v3.3.3) as described in Isaac et al. (2017), https://doi.org/10.5194/bg-14-2903-2017. PyFluxPro takes data recorded at the flux tower and process this data to a final, gap-filled product with Net Ecosystem Exchange (NEE) partitioned into Gross Primary Productivity (GPP) and Ecosystem Respiration (ER). For more information about the processing levels, see https://github.com/OzFlux/PyFluxPro/wiki. The Great Western Woodlands (GWW) comprise a 16 million hectare mosaic of temperate woodland, shrubland and mallee vegetation in south-west Western Australia. The region has remained relatively intact since European settlement, owing to the variable rainfall and lack of readily accessible groundwater. The woodland component is globally unique in that nowhere else do woodlands occur at as little as 220 mm mean annual rainfall. Further, other temperate woodlands around the world have typically become highly fragmented and degraded through agricultural use. The Great Western Woodlands Site was established in 2012 in the Credo Conservation Reserve. The site is in semi-arid woodland and was operated as a pastoral lease from 1907 to 2007. The core 1 ha plot is characterised by Eucalyptus salmonophloia (salmon gum), with Eucalyptus salubris and Eucalyptus clelandii dominating other research plots. The flux station is located in Salmon gum woodland. For additional site information, see https://www.tern.org.au/tern-observatory/tern-ecosystem-processes/great-western-woodlands-supersite/ . All flux raw data is subject to the quality control process OzFlux QA/QC to generate data from L1 to L6. Levels 3 to 6 are available for re-use. Datasets contain Quality Controls flags which will indicate when data quality is poor and has been filled from alternative sources. For more details, refer to Isaac et al (2017) in the Publications section, https://doi.org/10.5194/bg-14-2903-2017 .Progress Code: completedMaintenance and Update Frequency: notPlanned&rft.creator=Macfarlane, Craig &rft.creator=Prober, Suzanne &rft.creator=Wiehl, Georg &rft.date=2022&rft.edition=1.0&rft.relation=https://doi.org/10.5194/bg-14-2903-2017&rft.relation=https://doi.org/10.5194/bg-13-5895-2016&rft.relation=https://www.tern.org.au/tern-observatory/tern-ecosystem-processes/great-western-woodlands-supersite/&rft.coverage=Located in Credo Conservation Reserve, Western Australia&rft.coverage=northlimit=-30.1913; southlimit=-30.1913; westlimit=120.6541; eastLimit=120.6541; projection=EPSG:4326&rft_rights=Creative Commons Attribution 4.0 International Licence http://creativecommons.org/licenses/by/4.0&rft_rights=&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_subject=climatologyMeteorologyAtmosphere&rft_subject=BIOGEOCHEMICAL PROCESSES&rft_subject=EARTH SCIENCE&rft_subject=SOLID EARTH&rft_subject=GEOCHEMISTRY&rft_subject=LAND PRODUCTIVITY&rft_subject=LAND SURFACE&rft_subject=LAND USE/LAND COVER&rft_subject=EVAPOTRANSPIRATION&rft_subject=ATMOSPHERE&rft_subject=ATMOSPHERIC WATER VAPOR&rft_subject=TERRESTRIAL ECOSYSTEMS&rft_subject=BIOSPHERE&rft_subject=ATMOSPHERIC PRESSURE MEASUREMENTS&rft_subject=ATMOSPHERIC PRESSURE&rft_subject=TURBULENCE&rft_subject=WIND SPEED&rft_subject=WIND DIRECTION&rft_subject=TRACE GASES/TRACE SPECIES&rft_subject=ATMOSPHERIC CHEMISTRY&rft_subject=CARBON DIOXIDE&rft_subject=PHOTOSYNTHETICALLY ACTIVE RADIATION&rft_subject=LONGWAVE RADIATION&rft_subject=SHORTWAVE RADIATION&rft_subject=INCOMING SOLAR RADIATION&rft_subject=ATMOSPHERIC RADIATION&rft_subject=HEAT FLUX&rft_subject=AIR TEMPERATURE&rft_subject=ATMOSPHERIC TEMPERATURE&rft_subject=SURFACE TEMPERATURE&rft_subject=PRECIPITATION AMOUNT&rft_subject=PRECIPITATION&rft_subject=HUMIDITY&rft_subject=SOIL MOISTURE/WATER CONTENT&rft_subject=SOIL TEMPERATURE&rft_subject=ATMOSPHERIC SCIENCES&rft_subject=EARTH SCIENCES&rft_subject=ECOLOGICAL APPLICATIONS&rft_subject=ENVIRONMENTAL SCIENCES&rft_subject=Ecosystem Function&rft_subject=ENVIRONMENTAL SCIENCE AND MANAGEMENT&rft_subject=Environmental Monitoring&rft_subject=SOIL SCIENCES&rft_subject=Great Western Woodlands Flux Station&rft_subject=Middleton CN3&rft_subject=Campbell Scientific TCAV Averaging Soil Thermocouple Probe&rft_subject=LI-COR LI-7500&rft_subject=Kipp&Zonen CNR1&rft_subject=Kipp&Zonen NR Lite2&rft_subject=HyQuest Solutions CS700&rft_subject=Campbell Scientific CS616&rft_subject=Campbell Scientific CSAT3&rft_subject=air temperature&rft_subject=downward heat flux at ground level in soil&rft_subject=eastward wind&rft_subject=ecosystem respiration&rft_subject=gross primary productivity of biomass expressed as carbon&rft_subject=magnitude of surface downward stress&rft_subject=mass concentration of carbon dioxide in air&rft_subject=mass concentration of water vapor in air&rft_subject=mole fraction of carbon dioxide in air&rft_subject=mole fraction of water vapor in air&rft_subject=monin-obukhov length&rft_subject=net ecosystem exchange&rft_subject=net ecosystem productivity&rft_subject=northward wind&rft_subject=relative humidity&rft_subject=soil temperature&rft_subject=specific humidity&rft_subject=specific humidity saturation deficit in air&rft_subject=surface air pressure&rft_subject=surface downwelling longwave flux in air&rft_subject=surface downwelling shortwave flux in air&rft_subject=surface friction velocity&rft_subject=surface net downward radiative flux&rft_subject=surface upward flux of available energy&rft_subject=surface upward latent heat flux&rft_subject=surface upward mole flux of carbon dioxide&rft_subject=surface upward sensible heat flux&rft_subject=surface upwelling longwave flux in air&rft_subject=surface upwelling shortwave flux in air&rft_subject=thickness of rainfall amount&rft_subject=upward mole flux of carbon dioxide due inferred from storage&rft_subject=vertical wind&rft_subject=volume fraction of condensed water in soil&rft_subject=water evapotranspiration flux&rft_subject=water vapor partial pressure in air&rft_subject=water vapor saturation deficit in air&rft_subject=wind from direction&rft_subject=wind speed&rft_subject=Point Resolution&rft_subject=1 minute - < 1 hour&rft_subject=Eddy Covariance&rft_subject=AU-GWW&rft_subject=sparse eucalypt woodland&rft.type=dataset&rft.language=English Access the data

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Creative Commons Attribution 4.0 International Licence
http://creativecommons.org/licenses/by/4.0

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

Access:

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Contact Information

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Terrestrial Ecosystem Research Network
Building 1019, 80 Meiers Rd
QLD 4068
Australia
Ph: +61 7 3365 9097

esupport@tern.org.au

Brief description

This data release consists of flux tower measurements of the exchange of energy and mass between the surface and the atmospheric boundary-layer in semi-arid eucalypt woodland using eddy covariance techniques. It been processed using PyFluxPro (v3.3.3) as described in Isaac et al. (2017), https://doi.org/10.5194/bg-14-2903-2017. PyFluxPro takes data recorded at the flux tower and process this data to a final, gap-filled product with Net Ecosystem Exchange (NEE) partitioned into Gross Primary Productivity (GPP) and Ecosystem Respiration (ER). For more information about the processing levels, see https://github.com/OzFlux/PyFluxPro/wiki.

The Great Western Woodlands (GWW) comprise a 16 million hectare mosaic of temperate woodland, shrubland and mallee vegetation in south-west Western Australia. The region has remained relatively intact since European settlement, owing to the variable rainfall and lack of readily accessible groundwater. The woodland component is globally unique in that nowhere else do woodlands occur at as little as 220 mm mean annual rainfall. Further, other temperate woodlands around the world have typically become highly fragmented and degraded through agricultural use. The Great Western Woodlands Site was established in 2012 in the Credo Conservation Reserve. The site is in semi-arid woodland and was operated as a pastoral lease from 1907 to 2007. The core 1 ha plot is characterised by Eucalyptus salmonophloia (salmon gum), with Eucalyptus salubris and Eucalyptus clelandii dominating other research plots. The flux station is located in Salmon gum woodland. For additional site information, see https://www.tern.org.au/tern-observatory/tern-ecosystem-processes/great-western-woodlands-supersite/ .

Lineage

All flux raw data is subject to the quality control process OzFlux QA/QC to generate data from L1 to L6. Levels 3 to 6 are available for re-use. Datasets contain Quality Controls flags which will indicate when data quality is poor and has been filled from alternative sources. For more details, refer to Isaac et al (2017) in the Publications section, https://doi.org/10.5194/bg-14-2903-2017 .

Progress Code: completed
Maintenance and Update Frequency: notPlanned

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.
The Great Western Woodlands Site was established in 2012 and is managed by CSIRO Land and Water and funded by TERN and the WA Department of Environment and Conservation. The flux station is part of the Australia OzFlux Network and contributes to the international FLUXNET Network.
Purpose
The flux station and site work towards building a process-based understanding of semi-arid woodlands to inform management and climate adaptation in the Great Western Woodlands and climate-resilient restoration in the adjacent WA wheatbelt.
Data Quality Information

Data Quality Assessment Scope
local : dataset
If the data quality is poor, the data is filled from alternative sources. Filled data can be identified by the Quality Controls flags in the dataset. Quality control checks include (i) range checks for plausible limits, (ii) spike detection, (iii) dependency on other variables and (iv) manual rejection of date ranges. Specific checks applied to the sonic and IRGA data include 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. For more details, refer to Isaac et al (2017) in the Publications section, https://doi.org/10.5194/bg-14-2903-2017. For further information about the software (PyFluxPro) used to process and quality control the flux data, see https://github.com/OzFlux/PyFluxPro/wiki .

Created: 2022-03-17

Issued: 2022-03-28

Modified: 2014-07-14

Data time period: 2013-01-01 to 2022-01-01

This dataset is part of a larger collection

Click to explore relationships graph

120.6541,-30.1913

120.6541,-30.1913

text: Located in Credo Conservation Reserve, Western Australia

Subjects
1 minute - < 1 hour | AIR TEMPERATURE | ATMOSPHERE | ATMOSPHERIC CHEMISTRY | ATMOSPHERIC PRESSURE | ATMOSPHERIC PRESSURE MEASUREMENTS | ATMOSPHERIC RADIATION | Atmospheric Sciences | ATMOSPHERIC TEMPERATURE | ATMOSPHERIC WATER VAPOR | AU-GWW | BIOGEOCHEMICAL PROCESSES | BIOSPHERE | CARBON DIOXIDE | Campbell Scientific CS616 | Campbell Scientific CSAT3 | Campbell Scientific TCAV Averaging Soil Thermocouple Probe | EARTH SCIENCE | Earth Sciences | Ecological Applications | Environmental Science and Management | Environmental Sciences | EVAPOTRANSPIRATION | Ecosystem Function | Eddy Covariance | Environmental Monitoring | GEOCHEMISTRY | Great Western Woodlands Flux Station | HEAT FLUX | HUMIDITY | HyQuest Solutions CS700 | INCOMING SOLAR RADIATION | Kipp&Zonen CNR1 | Kipp&Zonen NR Lite2 | LAND PRODUCTIVITY | LAND SURFACE | LAND USE/LAND COVER | LI-COR LI-7500 | LONGWAVE RADIATION | Middleton CN3 | PHOTOSYNTHETICALLY ACTIVE RADIATION | PRECIPITATION | PRECIPITATION AMOUNT | Point Resolution | SHORTWAVE RADIATION | SOIL MOISTURE/WATER CONTENT | Soil Sciences | SOIL TEMPERATURE | SOLID EARTH | SURFACE TEMPERATURE | TERRESTRIAL ECOSYSTEMS | TRACE GASES/TRACE SPECIES | TURBULENCE | WIND DIRECTION | WIND SPEED | air temperature | climatologyMeteorologyAtmosphere | downward heat flux at ground level in soil | eastward wind | ecosystem respiration | gross primary productivity of biomass expressed as carbon | magnitude of surface downward stress | mass concentration of carbon dioxide in air | mass concentration of water vapor in air | mole fraction of carbon dioxide in air | mole fraction of water vapor in air | monin-obukhov length | net ecosystem exchange | net ecosystem productivity | northward wind | relative humidity | soil temperature | sparse eucalypt woodland | specific humidity | specific humidity saturation deficit in air | surface air pressure | surface downwelling longwave flux in air | surface downwelling shortwave flux in air | surface friction velocity | surface net downward radiative flux | surface upward flux of available energy | surface upward latent heat flux | surface upward mole flux of carbon dioxide | surface upward sensible heat flux | surface upwelling longwave flux in air | surface upwelling shortwave flux in air | thickness of rainfall amount | upward mole flux of carbon dioxide due inferred from storage | vertical wind | volume fraction of condensed water in soil | water evapotranspiration flux | water vapor partial pressure in air | water vapor saturation deficit in air | wind from direction | wind speed |

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