Data

Adelaide River Flux Data Release 2022_v1

Terrestrial Ecosystem Research Network
Beringer, Jason ; Hutley, Lindsay
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/qyp1-g447&rft.title=Adelaide River Flux Data Release 2022_v1&rft.identifier=10.25901/qyp1-g447&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 ecosystem was dominated by Eucalyptus tectifica and Planchonia careya . Elevation of the site was close to 90m and mean annual precipitation at a nearby Bureau of Meteorology site was 1730mm. Maximum temperatures ranged from 31.4°C (in June) to 36.8°C (in October) while minimum temperatures range from 16.2°C (in July) to 25.1°C (in December). Maximum temperature varied seasonally by approximately 5.4°C and minimum temperatures varied by approximately 8.9°C.The instrument mast was 15 meters tall. Heat, water vapour and carbon dioxide measurements were taken using the open-path eddy flux technique. Temperature, humidity, wind speed, wind direction, rainfall, incoming and reflected shortwave radiation and net radiation were measured above the canopy. Soil heat fluxes are measured and soil moisture content was gathered using time domain reflectometry. 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=Beringer, Jason &rft.creator=Hutley, Lindsay &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.coverage=Approximately 10.5km south east of Bachelor, Northern Territory&rft.coverage=northlimit=-13.0769; southlimit=-13.0769; westlimit=131.1178; eastLimit=131.1178; 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 /><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=ATMOSPHERIC 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=Adelaide River Flux Station&rft_subject=Kipp&Zonen CNR4&rft_subject=HyQuest Solutions CS700&rft_subject=Campbell Scientific CSAT3&rft_subject=LI-COR LI-7500&rft_subject=mole fraction of water vapor in air (Millimoles per mole)&rft_subject=Millimoles per mole&rft_subject=mole fraction of carbon dioxide in air (Micromoles per mole)&rft_subject=Micromoles per mole&rft_subject=surface upward latent heat flux (Watt per Square Meter)&rft_subject=Watt per Square Meter&rft_subject=downward heat flux at ground level in soil (Watt per Square Meter)&rft_subject=surface downwelling longwave flux in air (Watt per Square Meter)&rft_subject=surface upwelling longwave flux in air (Watt per Square Meter)&rft_subject=surface downwelling shortwave flux in air (Watt per Square Meter)&rft_subject=surface upwelling shortwave flux in air (Watt per Square Meter)&rft_subject=thickness of rainfall amount (Millimetre)&rft_subject=Millimetre&rft_subject=relative humidity (Percent)&rft_subject=Percent&rft_subject=specific humidity (Kilogram per Kilogram)&rft_subject=Kilogram per Kilogram&rft_subject=air temperature (degree Celsius)&rft_subject=degree Celsius&rft_subject=soil temperature (degree Celsius)&rft_subject=water vapor partial pressure in air (Kilopascal)&rft_subject=Kilopascal&rft_subject=water vapor saturation deficit in air (Kilopascal)&rft_subject=wind from direction (Degree)&rft_subject=Degree&rft_subject=wind speed (Meter per Second)&rft_subject=Meter per Second&rft_subject=surface air pressure (Kilopascal)&rft_subject=ecosystem respiration (Micromoles per square metre second)&rft_subject=Micromoles per square metre second&rft_subject=gross primary productivity of biomass expressed as carbon (Micromoles per square metre 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 Meter)&rft_subject=Gram per Cubic Meter&rft_subject=Monin-Obukhov length (Meter)&rft_subject=Meter&rft_subject=net ecosystem exchange (Micromoles per square metre second)&rft_subject=net ecosystem productivity (Micromoles per square metre second)&rft_subject=specific humidity saturation deficit in air (Kilogram per Kilogram)&rft_subject=surface friction velocity (Meter per Second)&rft_subject=surface upward flux of available energy (Watt per Square Meter)&rft_subject=surface net downward radiative flux (Watt per Square Meter)&rft_subject=surface upward mole flux of carbon dioxide (Micromoles per square metre second)&rft_subject=surface upward sensible heat flux (Watt per Square Meter)&rft_subject=upward mole flux of carbon dioxide due inferred from storage (Micromoles per square metre second)&rft_subject=volume fraction of condensed water in soil (Cubic Meter per Cubic Meter)&rft_subject=Cubic Meter per Cubic Meter&rft_subject=water evapotranspiration flux (Kilograms per square metre per second)&rft_subject=Kilograms per square metre per second&rft_subject=mass concentration of carbon dioxide in air (Milligram per Cubic Meter)&rft_subject=Milligram per Cubic Meter&rft_subject=Point Resolution&rft_subject=1 minute - < 1 hour&rft_subject=AU-Ade&rft_subject=Eddy Covariance&rft_subject=woody savanna&rft.type=dataset&rft.language=English Access the data

Licence & Rights:

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CC-BY

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:

Open view details

unclassified

Contact Information

Street Address:
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 ecosystem was dominated by Eucalyptus tectifica and Planchonia careya .

Elevation of the site was close to 90m and mean annual precipitation at a nearby Bureau of Meteorology site was 1730mm. Maximum temperatures ranged from 31.4°C (in June) to 36.8°C (in October) while minimum temperatures range from 16.2°C (in July) to 25.1°C (in December). Maximum temperature varied seasonally by approximately 5.4°C and minimum temperatures varied by approximately 8.9°C.The instrument mast was 15 meters tall. Heat, water vapour and carbon dioxide measurements were taken using the open-path eddy flux technique. Temperature, humidity, wind speed, wind direction, rainfall, incoming and reflected shortwave radiation and net radiation were measured above the canopy. Soil heat fluxes are measured and soil moisture content was gathered using time domain reflectometry.

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 site was established in November 2007 and was managed by Monash University and Charles Darwin University until it was decommissioned in May 2009. The station was part of OzFlux, the Australia Flux Network and contributed data to the international FLUXNET Network.
Purpose
The purpose of the Adelaide River Flux Station was to:
Provide information as part of a larger network of flux stations established along the North Australian Tropical Transect (NATT) gradient, which extends ~1000km south from Darwin 12.5°S.
Examine spatial patterns and processes of land-surface-atmosphere exchanges (radiation, heat, moisture, CO2 and other trace gasses) across scales from leaf to landscape scales within Australian savannas.
Determine the climate and ecosystem characteristics (physical structure, species composition, physiological function) that drive spatial and temporal variations of carbon, water and energy fluxes from north Australian savanna.
Determine if fluxes of carbon, water vapour and heat over the various ecosystems as derived from the various measurement techniques can be combined to form a comprehensive and consistent estimate of the regional fluxes and budgets across the landscape.
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: 2021-08-06

Issued: 2022-03-25

Modified: 2024-05-07

Data time period: 2007-10-17 to 2009-05-24

This dataset is part of a larger collection

Click to explore relationships graph

131.1178,-13.0769

131.1178,-13.0769

text: Approximately 10.5km south east of Bachelor, Northern Territory

Subjects
1 minute - < 1 hour | AIR TEMPERATURE | ATMOSPHERE | ATMOSPHERIC CARBON DIOXIDE | ATMOSPHERIC CHEMISTRY | ATMOSPHERIC PRESSURE | ATMOSPHERIC PRESSURE MEASUREMENTS | ATMOSPHERIC RADIATION | Atmospheric Sciences | ATMOSPHERIC TEMPERATURE | ATMOSPHERIC WATER VAPOR | AU-Ade | Adelaide River Flux Station | BIOGEOCHEMICAL PROCESSES | BIOSPHERE | Campbell Scientific CSAT3 | Cubic Meter per Cubic Meter | Degree | EARTH SCIENCE | Earth Sciences | Ecological Applications | Environmental Science and Management | Environmental Sciences | EVAPOTRANSPIRATION | Ecosystem Function | Eddy Covariance | Environmental Monitoring | GEOCHEMISTRY | Gram per Cubic Meter | HEAT FLUX | HUMIDITY | HyQuest Solutions CS700 | INCOMING SOLAR RADIATION | Kilogram per Kilogram | Kilograms per metre per square second | Kilograms per square metre per second | Kilopascal | Kipp&Zonen CNR4 | LAND PRODUCTIVITY | LAND SURFACE | LAND USE/LAND COVER | LI-COR LI-7500 | LONGWAVE RADIATION | Meter | Meter per Second | Micromoles per mole | Micromoles per square metre second | Milligram per Cubic Meter | Millimetre | Millimoles per mole | Monin-Obukhov length (Meter) | PHOTOSYNTHETICALLY ACTIVE RADIATION | PRECIPITATION | PRECIPITATION AMOUNT | Percent | 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 | Watt per Square Meter | air temperature (degree Celsius) | climatologyMeteorologyAtmosphere | degree Celsius | downward heat flux at ground level in soil (Watt per Square Meter) | ecosystem respiration (Micromoles per square metre second) | gross primary productivity of biomass expressed as carbon (Micromoles per square metre second) | magnitude of surface downward stress (Kilograms per metre per square second) | mass concentration of carbon dioxide in air (Milligram per Cubic Meter) | mass concentration of water vapor in air (Gram per Cubic Meter) | mole fraction of carbon dioxide in air (Micromoles per mole) | mole fraction of water vapor in air (Millimoles per mole) | net ecosystem exchange (Micromoles per square metre second) | net ecosystem productivity (Micromoles per square metre second) | relative humidity (Percent) | soil temperature (degree Celsius) | specific humidity (Kilogram per Kilogram) | specific humidity saturation deficit in air (Kilogram per Kilogram) | surface air pressure (Kilopascal) | surface downwelling longwave flux in air (Watt per Square Meter) | surface downwelling shortwave flux in air (Watt per Square Meter) | surface friction velocity (Meter per Second) | surface net downward radiative flux (Watt per Square Meter) | surface upward flux of available energy (Watt per Square Meter) | surface upward latent heat flux (Watt per Square Meter) | surface upward mole flux of carbon dioxide (Micromoles per square metre second) | surface upward sensible heat flux (Watt per Square Meter) | surface upwelling longwave flux in air (Watt per Square Meter) | surface upwelling shortwave flux in air (Watt per Square Meter) | thickness of rainfall amount (Millimetre) | upward mole flux of carbon dioxide due inferred from storage (Micromoles per square metre second) | volume fraction of condensed water in soil (Cubic Meter per Cubic Meter) | water evapotranspiration flux (Kilograms per square metre per second) | water vapor partial pressure in air (Kilopascal) | water vapor saturation deficit in air (Kilopascal) | wind from direction (Degree) | wind speed (Meter per Second) | woody savanna |

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