C
Cheng-I Hsieh
Researcher at National Taiwan University
Publications - 40
Citations - 2472
Cheng-I Hsieh is an academic researcher from National Taiwan University. The author has contributed to research in topics: Sensible heat & Turbulence. The author has an hindex of 25, co-authored 39 publications receiving 2343 citations. Previous affiliations of Cheng-I Hsieh include Duke University & National Taiwan University of Science and Technology.
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An approximate analytical model for footprint estimation of scalar fluxes in thermally stratified atmospheric flows
TL;DR: In this article, an approximate analytical model was developed to estimate scalar flux footprint in thermally stratified atmospheric surface layer flows based on a combination of Lagrangian stochastic dispersion model results and dimensional analysis.
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Estimating the uncertainty in annual net ecosystem carbon exchange: spatial variation in turbulent fluxes and sampling errors in eddy‐covariance measurements
Ram Oren,Cheng-I Hsieh,Cheng-I Hsieh,Paul C. Stoy,John D. Albertson,Heather R. McCarthy,P. A. Harrell,Gabriel G. Katul +7 more
TL;DR: In this paper, a spatial variability experiment, in which EC measurements were made from six towers within the roughness sublayer (RSL) in a uniform pine plantation, quantified large and dynamic spatial variation in fluxes.
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Estimation of surface heat and momentum fluxes using the flux-variance method above uniform and non-uniform terrain
TL;DR: In this article, the Monin and Obukhov (1954) variance similarity functions were compared with direct measurements for momentum and heat but not for water vapor, and it was demonstrated that the non-uniformity in water vapor sources reduced the surface flux when compared to an equivalent uniform terrain subjected to identical shear stress, sensible heat flux, and atmospheric water vapor variance.
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The ejection-sweep character of scalar fluxes in the unstable surface layer
TL;DR: In this article, the authors analyzed the ejection-sweep properties using velocity and scalar fluctuation measurements over tall natural grass and bare soil surfaces and showed that momentum ejections and sweeps occur at equal frequencies (D eject ≈ D sweep ≈ 0.29) irrespective of surfaceroughness length or atmospheric stability conditions.
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Turbulent eddy motion at the forest‐atmosphere interface
TL;DR: In this paper, the authors analyzed the ejection-sweep properties at the canopy-atmosphere interface of a 13 m tall, uniformly aged southern loblolly pine stand and a 33m tall, unevenly aged hardwood stand using velocity and scalar (temperature, water vapor, and carbon dioxide) fluctuation measurements.