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Ocean Color Indices of Frontal Boundary Movements: A Multi-Sensor View. [PDF]
Sensors (Basel)Jolliff JK +3 more
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Capturing the pace of extreme diurnal temperature change in climate-health assessment. [PDF]
Eco Environ HealthMa X, Wang J.
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On similarity in the atmospheric boundary layer
Boundary-Layer Meteorology, 1986A similarity theory for the atmospheric boundary layer is presented. The Monin-Obukhov similarity theory for the surface layer is a particular case of this new theory, for the case of z → 0. Universal functions which are in agreement with empirical data are obtained for the stable and convective regimes.
Zbigniew Sorbjan
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Atmospheric Boundary Layer Research at Cabauw
Boundary-Layer Meteorology, 1996At Cabauw, The Netherlands, a 213 m high mast specifically built for meteorological research has been operational since 1973. Its site, construction, instrumentation and observation programs are reviewed. Regarding analysis of the boundary layer at Cabauw, the following subjects are discussed: terrain roughness; Monin—Obukhov theory in ...
van Ulden, A.P., Wieringa, J.
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Applied Mechanics and Materials, 2016
Atmospheric Boundary Layer (ABL) is the lowest part of the troposphere. The main feature of the Atmospheric Boundary Layer is the turbulent nature of the flow. The thickness of the boundary layer, formed by flowing air friction on the earth’s surface under various conditions move in quite a wide range. ABL is generally defined as being 0.5 km above the
Andrea Vranková, Milan Palko
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Atmospheric Boundary Layer (ABL) is the lowest part of the troposphere. The main feature of the Atmospheric Boundary Layer is the turbulent nature of the flow. The thickness of the boundary layer, formed by flowing air friction on the earth’s surface under various conditions move in quite a wide range. ABL is generally defined as being 0.5 km above the
Andrea Vranková, Milan Palko
openaire +1 more source
Turbulence in the Atmospheric Boundary Layer
The Physics of Fluids, 1967The specific features of atmospheric boundary-layer turbulence are described. The small-scale properties of atmospheric turbulence depend very little on the peculiarities of its large-scale components and obey approximately the laws of locally isotropic turbulence. It is shown that turbulence is locally axisymmetric in respect to the vertical direction
openaire +2 more sources