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Santa Rita Mesquite
1055-Santa Rita Mesquite
An empirical model simulating diurnal and seasonal CO<sub>2</sub> flux for diverse vegetation types and climate conditions
Atqasuk
Audubon Research Ranch
Barrow
Bartlett Experimental Forest
Brookings
Donaldson
Duke Forest Hardwoods
Duke Forest Loblolly Pine
Duke Forest Open Field
Harvard Forest EMS Tower (HFR1)
Howland Forest (Main Tower)
Intermediate hardwood (IHW)
Ivotuk
Kennedy Space Center (scrub oak)
Mature red pine (MRP)
Metolius Intermediate Pine
Missouri Ozark Site
Mixed young jack pine (MYJP)
Park Falls
Santarem-Km67-Primary Forest
Santa Rita Mesquite
UCI 1850
UCI 1930
Walnut River Watershed
Saito, M.
,
Maksyutov S.
,
Hirata R.
, &
Richardson A. D.
(2009).
An empirical model simulating diurnal and seasonal CO
2
flux for diverse vegetation types and climate conditions
.
Biogeosciences. 6
(4), 585 - 599.
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Evidence for decadal variation in global terrestrial evapotranspiration between 1982 and 2002: 1. Model development
ARM Southern Great Plains site
Audubon Research Ranch
Bondville
British Columbia- Campbell River - Young Plantation Site
Brookings
Delta Junction 1920 Control site
Delta Junction 1987 Burn site
Delta Junction 1999 Burn site
Donaldson
Fermi National Accelerator Laboratory - (Agricultural site)
Fermi National Accelerator Laboratory - (Prairie site)
Freeman Ranch- Mesquite Juniper
Goodwin Creek
Haibei Meadow
Howard Springs
Ivotuk
Kennedy Space Center (scrub oak)
Mase Paddy (participated in AsiaFlux activities from 1999);
Maun- Mopane Woodland
Mead - irrigated continuous maize site
Mead - irrigated maize-soybean rotation site
Mead - rainfed maize-soybean rotation site
Missouri Ozark Site
Mize
Niwot Ridge (LTER NWT1)
Palangkaraya
Park Falls
Santa Rita Mesquite
Seebodenalp
Tomakomai National Forest
Tumbarumba
UCI 1850
UCI 1930
UCI 1964
UCI 1981
UCI 1989
UCI 1998
Walker Branch Watershed
Wallaby Creek
Walnut Gulch Kendall Grasslands
Walnut Gulch Lucky Hills Shrub
Willow Creek
Wang, K.
,
Dickinson R. E.
,
Wild M.
, &
Liang S.
(2010).
Evidence for decadal variation in global terrestrial evapotranspiration between 1982 and 2002: 1. Model development
.
Journal of Geophysical Research. 115
(D20),
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Santa Rita Mesquite Site Gallery
Santa Rita Mesquite
Pictures from the Santa Rita Mesquite FLUXNET tower site.
SpecNet revisited: bridging flux and remote sensing communities
Abisko
Atqasuk
Barrow
Bartlett Experimental Forest
British Columbia- Campbell River - Mature Forest Site
Chamela Biological Station
Duke Forest Hardwoods
Duke Forest Loblolly Pine
Fajemyr (NECC);
Hyytiala
Lethbridge
Lewis Springs Mesquite
Los Inocentes
Manhattan (cedar forest 30 km N);
Mead - irrigated continuous maize site
Monte Bondone
Morgan Monroe State Forest
Norunda
San Joaquin Freshwater Marsh, Tower 1
Santa Rita Mesquite
Santa Rosa National Park
Sask- SSA Old Aspen
Sky Oaks
Sky Oaks- Old Stand
Sky Oaks- Young Stand
Southern California Climate Gradient Coastal Sage
Stordalen Grassland (Mire);
Tumbarumba
Western Peatland- LaBiche-Black Spruce/Larch Fen
Gamon, J. A.
,
Coburn C.
,
Flanagan L. B.
,
Heummrich K. M.
,
Kiddle C.
,
Sanchez-Azofeifa G. A.
, et al.
(2010).
SpecNet revisited: bridging flux and remote sensing communities
.
Canadian Journal of Remote Sensing. 36
(supplement S2), S376-S390.
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The relative controls of temperature, soil moisture, and plant functional group on soil CO <sub>2</sub> efflux at diel, seasonal, and annual scales
Santa Rita Mesquite
Barron-Gafford, G. A.
,
Scott R. L.
,
Jenerette D. G.
, &
Huxman T. E.
(2011).
The relative controls of temperature, soil moisture, and plant functional group on soil CO
2
efflux at diel, seasonal, and annual scales
.
Journal of Geophysical Research. 116
(G1),
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Using watershed water balance to evaluate the accuracy of eddy covariance evaporation measurements for three semiarid ecosystems
Santa Rita Mesquite
Walnut Gulch Kendall Grasslands
Walnut Gulch Lucky Hills Shrub
Scott, R. L.
(2010).
Using watershed water balance to evaluate the accuracy of eddy covariance evaporation measurements for three semiarid ecosystems
.
Agricultural and Forest Meteorology. 150
(2), 219 - 225.
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