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Journal ArticleDOI

How Well Can We Measure the Vertical Wind Speed? Implications for Fluxes of Energy and Mass

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TLDR
In this article, wind-velocity measurement errors from a three-dimensional sonic anemometer with a non-orthogonal transducer orientation were estimated for over 100 combinations of angle-of-attack and wind direction using a novel technique to measure the true angle of attack and wind speed within the turbulent atmospheric surface layer.
Abstract
Sonic anemometers are capable of measuring the wind speed in all three dimen- sions at high frequencies (10-50 Hz), and are relied upon to estimate eddy-covariance-based fluxes of mass and energy over a wide variety of surfaces and ecosystems. In this study, wind-velocity measurement errors from a three-dimensional sonic anemometer with a non- orthogonal transducer orientation were estimated for over 100 combinations of angle-of- attack and wind direction using a novel technique to measure the true angle-of-attack and wind speed within the turbulent atmospheric surface layer. Corrections to the vertical wind speed varied from −5 to 37% for all angles-of-attack and wind directions examined. When applied to eddy-covariance data from three NOAA flux sites, the wind-velocity corrections increased the magnitude of CO2 fluxes, sensible heat fluxes, and latent heat fluxes by ≈11%, with the actual magnitude of flux corrections dependent upon sonic anemometer, surface type, and scalar. A sonic anemometer that uses vertically aligned transducers to measure the vertical wind speed was also tested at four angles-of-attack, and corrections to the ver- tical wind speed measured using this anemometer were within ±1% of zero. Sensible heat fluxes over a forest canopy measured using this anemometer were 15% greater than sensible heat fluxes measured using a sonic anemometer with a non-orthogonal transducer orienta- tion. These results indicate that sensors with a non-orthogonal transducer orientation, which includes the majority of the research-grade three-dimensional sonic anemometers currently in use, should be redesigned to minimize sine errors by measuring the vertical wind speed using one pair of vertically aligned transducers.

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Citations
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Journal ArticleDOI

Surface-Energy-Balance Closure over Land: A Review

TL;DR: In this paper, the authors provide an overview of the potential reason for the lack of closure of the energy balance closure problem, and address questions with regard to the partitioning of the residual energy balance residual between the sensible and latent fluxes.
Journal ArticleDOI

Towards a consistent eddy-covariance processing: an intercomparison of EddyPro and TK3

TL;DR: In this paper, a comparison of two popular eddy-covariance software packages, namely, EddyPro and TK3, is presented, and two approximately 1-month long test data sets were processed, representing typical instrumental setups (i.e., CSAT3/LI-7500 above grassland and Solent R3/ LI-6262 above a forest).
Journal ArticleDOI

Correction of a non-orthogonal, three-component sonic anemometer for flow distortion by transducer shadowing

TL;DR: In this article, the authors investigated the dependence of transducer shadowing on sonic path geometry, wind direction and atmospheric stability with simulations that use surface layer data from the Horizontal array Turbulence Study (HATS) field program and canopy roughness-sublayer data from CHATS field program.
Journal ArticleDOI

Underestimates of sensible heat flux due to vertical velocity measurement errors in non-orthogonal sonic anemometers

TL;DR: In this paper, the authors tested whether a non-orthogonal sonic anemometer (CSAT3, Campbell Scientific, Inc.) measures lower vertical wind velocity and sensible heat flux than an orthogonal anemometers (SATI/3Vx, Applied Technologies, Inc.).
References
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Journal ArticleDOI

Correction of flux measurements for density effects due to heat and water vapour transfer

TL;DR: In this article, the basic relationships are discussed in the context of vertical transfer in the lower atmosphere, and the required corrections to the measured flux are derived, where the correction to measurements of water vapour flux will often be only a few per cent but will sometimes exceed 10 percent.
Journal ArticleDOI

Temperature measurement with a sonic anemometer and its application to heat and moisture fluxes

TL;DR: In this paper, the possibility of measuring heat and moisture fluxes using sonic anemometer data is investigated, and theoretical relations for the temperature variance and heat flux are derived.
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