The Sturt Plains flux station is located approximately 280km north of Tennant Creek, Northern Territory. It was established in August 2008 and is managed by Monash University external and Charles Darwin University. The Sturt Plains OzFlux Site is located on a low lying plain dominated by Mitchell Grass (gen. Astrebla). Elevation of the site is close to 250m and mean annual precipitation at a nearby Bureau of Meteorology site is 640mm.Maximum temperatures range from 28.4°C (in June/ July) to 39.1°C (in December), while minimum temperatures range from 11.2°C (in July) to 24.4°C (in December).The instrument mast is 5 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 is gathered using time domain reflectometry.Ancillary measurements taken at the site include LAI, leaf-scale physiological properties (gas exchange, leaf isotope ratios, N and chlorophyll concentrations), vegetation optical properties and soil physical properties. Airborne based remote sensing (Lidar and hyperspectral measurements) was carried out across the transect in September 2008.
Flux measurements from the Cow Bay site, Far North Queensland.The Cow Bay flux station was located in the Daintree forest at the Daintree Discovery Centre, Cow Bay, 100km north of Cairns in Far North Queensland. It was established in December 2008 and managed by James Cook University.The forest is classified as complex mesophyll vine forest, there are 94 species in the core 1Ha, and average tree height is 22m. Elevation of the site is 90m and mean annual precipitation is 3935mm. The Daintree Rainforest is one of the most biodiverse forests in Australia.The instruments are mounted on a walk-up tourist tower at 35m. Fluxes of heat, water vapour and carbon dioxide are measured using the open-path eddy flux technique. Supplementary measurements above the canopy include temperature, humidity, windspeed, wind direction, rainfall, incoming and reflected shortwave radiation and net radiation.The early years 2009 - 12 had several data gaps. Shadowing of the radiometric equipment continues to cause artifacts on the radiometers - these can be seen as reduction in downwelling radiation with solar inclination. We are currently working on a hardware solution.The site is part of the FNQ Rainforest SuperSite : associated with the Daintree node, which is part of the TERN Australian SuperSite Network (ASN). The site was co-funded by the Daintree Discovery Centre and the Terrestrial Ecosystem Research Network. Past support was from the Department of Environment and Heritage - Marine and Tropical Sciences Research Facility Project 5ii.2. Climate Change: Scaling from trees to ecosystems.
Ecosystem flux data from the Adelaide River site, Northern Territory.The Adelaide River flux station was located approximately 10.5km south east of Bachelor, Northern Territory. The flux tower site was classified as Savanna 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 is 1730mm. Maximum temperatures range 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 vary seasonally by approximately 5.4°C and minimum temperatures vary 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.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 Daly River Uncleared flux tower site is located in the Douglas River Daly River Esplanade Conservation area, approximately 60 km south west of Pine Creek, Northern Territory (GPS coordinates: -14.1592, 131.3881).The flux tower site is classified as a Woodland savanna. The overstory is co dominated by tree species E. tetrodonta, C. latifolia, Terminalia grandiflora, Sorghum sp. and Heteropogon triticeus. Average canopy height measures 16.4 m. Elevation of the site is close to 110m and mean annual precipitation at a nearby Bureau of Meteorology site is 1170mm.Maximum temperatures range from 37.5°C (in October) to 31.2°C (in June), while minimum temperatures range from 12.6°C (in July) to 23.8°C (in January). Maximum temperatures range seasonally by 6.3°C and minimum temperatures by 11.2°C.The instrument mast is 23 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, incoming and reflected shortwave radiation and net radiation are measured above the canopy.Ancillary measurements taken at the site include LAI, leaf-scale physiological properties (gas exchange, leaf isotope ratios, N and chlorophyll concentrations), vegetation optical properties and soil physical properties. Airborne based remote sensing (Lidar and hyperspectral measurements) was carried out across the transect in September 2008.
Data from Wallaby Creek flux tower, Victoria.The Wallaby Creek flux station is located in Kinglake National Park, Victoria, South Eastern Australia. The area is assigned the IUCN Category II (National Parks) of the United Nations’ list of National Parks and protected areas, which means that park is primarily managed for ecosystem conservation.The site is approximately 45km north east of Melbourne, lies at an elevation of approximately 720 metres, and is located on the southern edge of the Hume Plateau. The catchment area is dominated by Eucalyptus Regnans or Mountain Ash, the world’s tallest flowering plant (angiosperm). Trees can reach heights of more than 90 metres growing in areas with high rainfall and fertile soil. These trees are well distributed throughout Victoria’s Central Highlands including the Otway Ranges and Strzlecki Ranges; they are also found in Tasmania. The site contains a chronosequence of (20, 80 and 300) stand ages that were established during fires occurring over the last 300 years.The tower itself is located within an old growth stand with individual trees as old as 300 years. Mountain ash forests are confined to the cool mountain regions with elevations ranging from 460 - 1100m and average rainfalls of 1100-2000mm. The forest is classed as a tall, wet sclerophyll forest, and the dominant Mountain Ash trees have an average canopy height of 75m. Below the dominant canopy lies a temperate rainforest understorey consisting of Pomaderris aspera and Olearia argophylla species, which are 10-18 metres tall. The lower layers of vegetation are dominated by tree ferns (Cyathea australis and Dicksonia antartica) and extensive tracts of rosette and rhizonic ferns (Polystichum proliferum and Blechnum wattsii) as well as Acacia trees.The catchment area contains a portion of the Mt Disappointment range, the Divide and the headwaters of Wallaby Creek and Silver Creek, and much of the slopes are characterised as flat to moderate.The major soil type within the forest is krasnozemic soils, which are friable red/brown, with high amounts of organic matter in the upper 20 – 30cm. However, the composition of krasnozemic soils is not homogenous, but rather a variation with altitude can be observed; lower altitudes inhabit grey-yellow podsolised soils compared to higher altitudes of the Kinglake and Hume plateau where the soil composition is krasnozemic loams. The clay content of these soils increases with depth until at least 200 cm deep, where after a transition soils contain rock fragments.The station was established in August 2005 by Monash University, operated in collaboration with Charles Darwin University and University of Alaska Faribanks. The original tower was destroyed in February 2009 by bushfires. Before the bushfire, the main mast stood at 110m. In March 2010, a replacement tower was established and sat at a height of 5m. Data from the site has been recorded from May 2010 onwards. As the tower is relatively new, the post fire instrumentation is currently not as diverse when compared to the pre fire instrumentation.The climate of the study area is classified as a cool, temperate zone, with the highest temperatures occurring during the summer months of December – February (13.8 – 22.5°C), whilst the coolest temperatures are experienced in May and August (4.7 – 9.2°C). Average annual precipitation is 1209mm, with a maximum rainfall occurring in June (Ashton, 2000). The study site experiences foggy conditions after sunset during autumn and winter.
The Cape Tribulation flux station is located in lowland tropical rainforest at the Daintree Rainforest Observatory located near Cape Tribulation, Queensland. The land is adjacent to the Daintree National Park which is part of the Wet Tropics World Heritage Area (WTWHA).The site is flanked to the west by coastal ranges rising to more than 1400m and to the east by the Coral Sea. The red clay loam podzolic soils are of metamorphic origin and have good drainage characteristics. The metamorphic rocks grade into granite boulders along Thompson Creek which runs along the northern boundary of the site. The crane site itself is gently sloping but the fetch area makes the site one of very complex terrain.The forest is classed as complex mesophyll vine forest (type 1a) and has an average canopy height of 25m. The dominant canopy trees belong to the Apocynaceae, Arecaceae, Euphorbiaceae, Lauraceae, Meliaceae, Myristicaceae and Myrtaceae families. The forest is continuous for several kilometres around the crane except for an area 300m due east of the crane, which is regrowth forest.Annual average rainfall at the site is around 5180mm and is strongly seasonal, with 66% falling between January and April (wet season). Mean daily temperature ranges from 26.6°C in February to 21.2°C in July.Tropical Cyclone impactsTropical cyclones are a frequent occurrence in Far North Queensland. These severe tropical storm systems are natural phenomena which play a major role in determining the ecology of Queensland's tropical lowland rainforests. In March 1999 Tropical Cyclone Rona (Category 3) passed over the Cape Tribulation area causing widespread damage (gusts >170km/h). At the site several large trees fell, nearly all of the remaining trees were stripped of leaves and the lianas towers were torn to ground level.Australian Canopy CraneThe flux station is mounted at the 45m level on the tower of the crane.The canopy crane is a Liebherr 91 EC, freestanding construction tower crane. The crane is 48.5 metres tall with a radius of 55 metres enabling access to 1 hectare of rainforest.Fluxes of heat, water vapour and carbon dioxide are measured using the open-path eddy covariance technique. Supplementary measurements above the canopy include temperature, humidity, rainfall, total solar, photosynthetically active radiation (PAR) and net radiation.Heat flux, soil temperature and water content (time domain reflectometry) are measured in proximity to the flux station. Detailed biometric measurements are made at the crane site and all trees have regular (5 yearly) dbh measurements and canopy mapping carried. Monitoring bores (3) are located on site. Leaf litter measurements are carried out on a monthly basis.The Cape Tribulation flux station was established in March 2001 and is managed by James Cook University.
The Wombat Forest research site is located in the Wombat State Forest, 100 km west of Melbourne Victoria, Australia (GPS coordinates: -37.4222, 144.0944; elevation: 713m).The site is a secondary re-growth forest that was last harvested in 1980. Dominant tree species are Eucalyptus obliqua (messmate stringybark), Eucalyptus radiata (narrow leaf peppermint) and Eucalyptus rubida (candlebark) with an average canopy height of 25m.The understorey consists mainly of patchy grasses and the soil is a silty-clay overlying clay. The forest is managed by the Department of Sustainability and Environment and management includes selective harvesting and prescribed burning regimes.The climate of the study area is classified as cool-temperate to Mediterranean zone with cold and wet winters (May-Aug) and warm and dry summers (Dec-Feb). Mean annual rainfall in the region in the last 20 years was between 600-700 mm.Measurement height: 35m from January 2017 (30m 2010 to 2016) Established in January 2010 and managed by The University of Melbourne in collaboration with Monash University and the Department of Sustainability and Environment of Victoria.
The Great Western Woodlands (GWW) comprise a 16 million hectare mosaic of temperate woodland, shrubland and mallee vegetation in south-west WA. The region is extraordinary in that it 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 flux site is located in Salmon gum (Eucalyptus salmonophloia) woodland in the northern part of the Great Western Woodlands at mean annual rainfall of c. 240 mm.The site was established in December 2012. It is located on Credo Station, 110km NNW of Kalgoorlie, WA, and is managed by the CSIRO Land and Water Flagship external link (Floreat).
The Fogg Dam flux station was located approximately 6km east of Black Jungle, Northern Territory. It was established in February 2006 and decommissioned in September 2008. It was managed by Monash University and Charles Darwin University.The site was situated within a wetland that flooded seasonally. The principle vegetation was Oryza rufipogon, Pseudoraphis spinescens and Eleocharis dulcis. The elevation was approximately 4m, with a neighbouring Bureau of Meteorology station recording 1411mm mean annual precipitation.Maximum temperatures ranged from 31.3°C (in June and July) to 35.6°C (in October), while minimum temperatures ranged from 14.9°C (in July) to 23.9°C (in December and February). Maximum temperatures varied on a seasonal basis by approximately 4.3°C and minimum temperatures by 9.0°C.The instrument mast was 15m tall. Heat, water vapour and carbon dioxide measurements are 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 were measured and soil moisture content was gathered using time domain reflectometry.Ancillary measurements taken at the site include LAI, leaf-scale physiological properties (gas exchange, leaf isotope ratios, N and chlorophyll concentrations), vegetation optical properties and soil physical properties. Airborne based remote sensing (Lidar and hyperspectral measurements) was carried out across the transect in September 2008.
The measurement site is located on Calperum Station. The site was established in July 2010 and is managed by the University of Adelaide (UA), coordinated by Prof Wayne Meyer and Prof David Chittleborough of the Landscape Futures Program as part of the Environment Institute.This is a former sheep grazing property that has been destocked and is being managed as a conservation area in this type of ecosystem. The landscape is flat with a series of low east–west sand dunes.The dunes are remnants of a previous dry era and are mostly now stabilised by mallee (multi-stemmed Eucalypt trees) and various shrubs. It is a semi-arid environment fringing the River Murray floodplains of the Riverland.