Results 31 to 40 of about 7,453 (161)

Does increased spatial replication above heterogeneous agroforestry improve the representativeness of eddy covariance measurements? [PDF]

open access: yesBiogeosciences
Spatial heterogeneity in terrestrial ecosystems compromises the accuracy of eddy covariance measurements. Examples of heterogeneous ecosystems are temperate agroforestry systems, which have been poorly studied by eddy covariance.
J. Á. Callejas-Rodelas   +8 more
doaj   +1 more source

Lag time determination in DEC measurements with PTR-MS [PDF]

open access: yesAtmospheric Measurement Techniques, 2010
The disjunct eddy covariance (DEC) method has emerged as a popular technique for micrometeorological flux measurements of volatile organic compounds (VOCs).
R. Taipale, T. M. Ruuskanen, J. Rinne
doaj   +1 more source

Improved processing methods for eddy covariance measurements in calculating sensible heat fluxes at glacier surfaces

open access: yesJournal of Glaciology
Bulk aerodynamic methods have been shown to perform poorly in computing turbulent heat fluxes at glacier surfaces during shallow katabatic winds. Katabatic surface layers have different wind shear and flux profiles to the surface layers for which the ...
Cole Lord-May, Valentina Radić
doaj   +1 more source

Modelling Amazonian forest eddy covariance data: a comparison of big leaf versus sun/shade models for the C-14 tower at Manaus I. Canopy photosynthesis [PDF]

open access: yesActa Amazonica, 2006
In this study, we concentrate on modelling gross primary productivity using two simple approaches to simulate canopy photosynthesis: "big leaf" and "sun/shade" models.
Lina Mercado   +5 more
doaj   +1 more source

High‐Latitude Eddy Covariance Temporal Network Design and Optimization

open access: yesJournal of Geophysical Research: Biogeosciences, 2023
Abstract Ecosystems at high latitudes are changing rapidly in response to climate change. To understand changes in carbon fluxes across seasonal to multi‐decadal timescales, long‐term in situ measurements from eddy covariance networks are needed. However, there are large spatiotemporal gaps in
Martijn Pallandt   +6 more
openaire   +2 more sources

Estimating scalar turbulent fluxes with slow-response sensors in the stable atmospheric boundary layer [PDF]

open access: yesAtmospheric Chemistry and Physics
Conventional and recently developed approaches for estimating turbulent scalar fluxes under stable atmospheric conditions are evaluated, with a focus on gases for which fast sensors are not readily available.
M. Allouche   +10 more
doaj   +1 more source

Howland Forest, ME, USA: Multi-Gas Flux (CO2, CH4, N2O) Social Cost Product Underscores Limited Carbon Proxies

open access: yesLand, 2021
Forest carbon sequestration is a widely accepted natural climate solution. However, methods to determine net carbon offsets are based on commercial carbon proxies or CO2 eddy covariance research with limited methodological comparisons. Non-CO2 greenhouse
Bruno D. V. Marino   +2 more
doaj   +1 more source

The use of disjunct eddy sampling methods for the determination of ecosystem level fluxes of trace gases [PDF]

open access: yesAtmospheric Chemistry and Physics, 2009
The concept of disjunct eddy sampling (DES) for use in measuring ecosystem-level micrometeorological fluxes is re-examined. The governing equations are discussed as well as other practical considerations and guidelines concerning this sampling method as ...
A. A. Turnipseed   +8 more
doaj  

On evapotranspiration and eddy covariance measurements corrections [PDF]

open access: yes, 2020
Abstract. Eddy Covariance (EC) technique is one of the most used technique monitoring Green House Gases (GHG) fluxes such as H2O, CO2, CH4. Water vapor movement and corresponding air density fluctuations were corrected by Webb et al. (1980) but not water vapor formation.
openaire   +2 more sources

Some aspects of the energy balance closure problem [PDF]

open access: yesAtmospheric Chemistry and Physics, 2006
After briefly discussing several reasons for the energy balance closure problem in the surface layer, the paper focuses on the influence of the low frequency part of the turbulence spectrum on the residual. Changes in the turbulent fluxes in this part of
T. Foken   +4 more
doaj  

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