Data

Cumberland Plain Flux Data Release 2022_v1

Terrestrial Ecosystem Research Network
Pendall, Elise ; Griebel, Anne ; Barton, Craig ; Metzen, Daniel
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/pb5z-v739&rft.title=Cumberland Plain Flux Data Release 2022_v1&rft.identifier=10.25901/pb5z-v739&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. The dataset has 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 Cumberland Plain flux station is located in a dry sclerophyll forest. The Cumberland Plain Woodland is now an endangered ecological community that encompasses distinct groupings of plants growing on clayey soils. The canopy is dominated by Eucalyptus moluccana and Eucalyptus fibrosa, which host an expanding population of mistletoe. Average canopy height is 23m, the elevation of the site is 20m and mean annual precipitation is 800mm. Fluxes of water vapour, carbon dioxide and heat are quantified with the open-path eddy flux technique from a 30 m tall mast. Additional measurements above the canopy include temperature, humidity, wind speed and direction, rainfall, incoming and reflected shortwave and longwave radiation and net, diffuse and direct radiation and the photochemical reflectance index. In addition, profiles of humidity and CO2 are measured at eight levels within the canopy, as well as measurements of soil moisture content, soil heat fluxes, soil temperature, and 10-hr fuel moisture dynamics. In addition, regular monitoring of understory species abundance, mistletoe infection, leaf area index and litterfall are also performed. For additional site information, see https://www.tern.org.au/tern-observatory/tern-ecosystem-processes/cumberland-plain-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=Pendall, Elise &rft.creator=Griebel, Anne &rft.creator=Barton, Craig &rft.creator=Metzen, Daniel &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/cumberland-plain-supersite/&rft.coverage=In the Hawkesbury Valley in central New South Wales.&rft.coverage=northlimit=-33.6152; southlimit=-33.6152; westlimit=150.7236; eastLimit=150.7236; 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=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=Cumberland Plain Flux Station&rft_subject=Campbell Scientific TCAV Averaging Soil Thermocouple Probe&rft_subject=LI-COR LI-7500&rft_subject=Kipp&Zonen CNR4&rft_subject=HyQuest Solutions CS700&rft_subject=LI-COR LI-840&rft_subject=Campbell Scientific CS616&rft_subject=Gill Windsonic4&rft_subject=Hukseflux HFP01&rft_subject=LI-COR LI-190SB&rft_subject=air temperature&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 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=downward heat flux at ground level in soil&rft_subject=surface downwelling photosynthetic photon flux in air&rft_subject=Point Resolution&rft_subject=1 minute - < 1 hour&rft_subject=eddy covariance&rft_subject=AU-Cum&rft_subject=dry sclerophyll forest&rft.type=dataset&rft.language=English Access the data

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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. The dataset has 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 Cumberland Plain flux station is located in a dry sclerophyll forest. The Cumberland Plain Woodland is now an endangered ecological community that encompasses distinct groupings of plants growing on clayey soils. The canopy is dominated by Eucalyptus moluccana and Eucalyptus fibrosa, which host an expanding population of mistletoe. Average canopy height is 23m, the elevation of the site is 20m and mean annual precipitation is 800mm.

Fluxes of water vapour, carbon dioxide and heat are quantified with the open-path eddy flux technique from a 30 m tall mast. Additional measurements above the canopy include temperature, humidity, wind speed and direction, rainfall, incoming and reflected shortwave and longwave radiation and net, diffuse and direct radiation and the photochemical reflectance index. In addition, profiles of humidity and CO2 are measured at eight levels within the canopy, as well as measurements of soil moisture content, soil heat fluxes, soil temperature, and 10-hr fuel moisture dynamics. In addition, regular monitoring of understory species abundance, mistletoe infection, leaf area index and litterfall are also performed.
For additional site information, see https://www.tern.org.au/tern-observatory/tern-ecosystem-processes/cumberland-plain-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 flux station is managed by the Hawkesbury Institute for the Environment at Western Sydney University and was funded by the Education Investment Fund and TERN.
Purpose
The purpose of the Cumberland Plain flux station is:
to quantify the exchanges of carbon dioxide, water vapour and energy in a dry sclerophyll forest.
to characterize the functional behaviour and sensitivity of the different components contributing to the ecosystem carbon balance from sub-daily to multi-annual temporal scales and under climatic variability.
to identify the role of hydraulic limitations on constraining ecosystem productivity.
to quantify the impact of mistletoe on plant physiological processes and whole ecosystem water vapour and carbon dioxide exchange.
to validate remote sensing estimates of different radiation components to obtain accurate regional predictions of fuel moisture.
to understand how wood traits and microbial diversity interact to determine rates of wood decay.
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: 2022-03-27

Modified: 2014-07-14

Data time period: 2014-01-01 to 2022-01-01

This dataset is part of a larger collection

Click to explore relationships graph

150.7236,-33.6152

150.7236,-33.6152

text: In the Hawkesbury Valley in central New South Wales.

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-Cum | BIOGEOCHEMICAL PROCESSES | BIOSPHERE | CARBON DIOXIDE | Campbell Scientific CS616 | Campbell Scientific TCAV Averaging Soil Thermocouple Probe | Cumberland Plain Flux Station | EARTH SCIENCE | Earth Sciences | Ecological Applications | Environmental Science and Management | Environmental Sciences | EVAPOTRANSPIRATION | Ecosystem Function | Environmental Monitoring | GEOCHEMISTRY | Gill Windsonic4 | HEAT FLUX | HUMIDITY | Hukseflux HFP01 | HyQuest Solutions CS700 | INCOMING SOLAR RADIATION | Kipp&Zonen CNR4 | LAND PRODUCTIVITY | LAND SURFACE | LAND USE/LAND COVER | LI-COR LI-190SB | LI-COR LI-7500 | LI-COR LI-840 | LONGWAVE RADIATION | 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 | dry sclerophyll forest | eastward wind | ecosystem respiration | eddy covariance | gross primary productivity of biomass expressed as carbon | magnitude of surface downward stress | 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 | specific humidity | specific humidity saturation deficit in air | surface air pressure | surface downwelling longwave flux in air | surface downwelling photosynthetic photon 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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