Works matching IS 00068314 AND DT 2012 AND VI 145 AND IP 2
Results: 7
How Well Can We Measure the Vertical Wind Speed? Implications for Fluxes of Energy and Mass.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 383, doi. 10.1007/s10546-012-9738-1
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A Method for Increasing the Turbulent Kinetic Energy in the Mellor-Yamada-Janjić Boundary-Layer Parametrization.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 329, doi. 10.1007/s10546-012-9727-4
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- Article
Consistent Two-Equation Closure Modelling for Atmospheric Research: Buoyancy and Vegetation Implementations.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 307, doi. 10.1007/s10546-012-9726-5
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- Article
On the Scaling Laws of the Velocity-Scalar Cospectra in the Canopy Sublayer Above Tall Forests.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 351, doi. 10.1007/s10546-012-9737-2
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Towards Reconciling the Large-Scale Structure of Turbulent Boundary Layers in the Atmosphere and Laboratory.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 273, doi. 10.1007/s10546-012-9735-4
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A New Eddy-Covariance Method Using Empirical Mode Decomposition.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 369, doi. 10.1007/s10546-012-9741-6
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- Article
Corrections to the Mathematical Formulation of a Backwards Lagrangian Particle Dispersion Model.
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- Boundary-Layer Meteorology, 2012, v. 145, n. 2, p. 399, doi. 10.1007/s10546-012-9739-0
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- Article