
doi: 10.1007/bf00713146
The spatial resolution of meteorological observations of scalars (such as concentrations or temperature) and scalar fluxes (e.g., water-vapour flux, sensible heat flux) above inhomogeneous surfaces is in general not known. It is determined by the surface area of influence orsource area of the sensor, which for sensors of quantities that are subject to turbulent diffusion, depends on the flow and turbulence conditions.
Earth sciences, info:eu-repo/classification/ddc/550, 550, ddc:550
Earth sciences, info:eu-repo/classification/ddc/550, 550, ddc:550
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