Field intercomparison of four methane gas analyzers suitable for eddy
covariance flux measurements
Eddy -
covariance flux towers are also funded by national programmes.
However, Helbig et al. [2017], using a set of nested paired eddy
covariance flux towers in a boreal forest - wetland landscape, point to the increasing importance of warming temperatures on ecosystem respiration potentially overwhelming enhanced productivity occurring from land cover change under projected anthropogenic trends.
Celis et al., 2017 combined six years of eddy
covariance flux tower data and soil respiration chambers and found that a moist tundra site was a source of carbon to the atmosphere, but much of the net source arises from the slow, but continuous emissions in winter.
Our key tools are instrumentation that observe the atmosphere (eddy -
covariance flux stations, lidar, sodar, ceilometers, scintillometers, infra - red cameras).
Not exact matches
The tower is part of the AmeriFlux network, a consortium of scientists using a network to work with the eddy
covariance technique, measuring
fluxes of CO2 and CH4 at multiple sites across the Americas.
Ocean heat
flux is a turbulent and complex system [7] which utilizes atmospheric measurement techniques such as eddy
covariance to measure the rate of heat transfer expressed in the unit of joules or watts per second.
The eddy
covariance observations and the model simulations over Europe illustrate the fact that there is a larger correlation of
flux changes with rainfall than with temperature changes.
Workshop participants recommended that steps should be taken to define air - sea
fluxes as ECVs or EOVs, particularly for those
fluxes that can be measured directly and for which there is consensus about measurement methods (e.g., air - sea heat and momentum exchanges using the eddy
covariance method).
In the majority of cases, ebullition was measured with funnels or was lumped with diffusive
flux via floating chamber measurements; however, in two studies, researchers estimated methane
fluxes via eddy
covariance (Eugster et al. 2011, Deshmukh et al. 2014), and in another two studies, researchers estimated ebullitive
flux via acoustic methods (DelSontro et al. 2011, 2015).
Aquatic GHG
fluxes are measured using a variety of techniques (e.g., floating chambers, thin boundary methods, eddy
covariance towers, acoustic methods, and funnels; supplemental figure S1) that provide varying degrees of spatial and temporal coverage and accuracy (St. Louis et al. 2000).
Although we did not explicitly address the temporal or spatial resolution of emission data from each system, it is notable that the few published acoustic and eddy
covariance - based reservoir CH4
flux estimates are quite high compared to the median CH4
flux estimates from less temporally and / or spatially integrated measurement techniques (figure 1).
Ecosystem - atmosphere CO2 exchange on short time - scales can be measured using micrometeorological techniques such as eddy
covariance, which relies on rapidly responding sensors mounted on towers to resolve the net
flux of CO2 between a patch of land and the atmosphere (Baldocchi et al., 1988).
Lasslop, G., Reichstein, M., Detto, M., Richardson, A. D. & Baldocchi, D. D. Comment on Vickers et al: Self - correlation between assimilation and respiration resulting from
flux partitioning of eddy -
covariance CO2
fluxes.
Vickers, D., Thomas, C. K., Martin, J. G. & Law, B. Self - correlation between assimilation and respiration resulting from
flux partitioning of eddy -
covariance CO2
fluxes.