Zobrazeno 1 - 10
of 37
pro vyhledávání: '"K. G. McNAUGHTON"'
Publikováno v:
Nonlinear Processes in Geophysics, Vol 14, Iss 3, Pp 257-271 (2007)
We report velocity and temperature spectra measured at nine levels from 1.42 meters up to 25.7 m over a smooth playa in Western Utah. Data are from highly convective conditions when the magnitude of the Obukhov length (our proxy for the depth of the
Externí odkaz:
https://doaj.org/article/15b5c476dbb144059fb8b1cc83d40853
Publikováno v:
Hydrology and Earth System Sciences, Vol 1, Iss 1, Pp 81-91 (1997)
Values of the momentum roughness length, z0, and displacement height, d, derived from wind profiles and momentum flux measurements, are selected from the literature for a variety of sparse canopies. These include savannah, tiger-bush and several row
Externí odkaz:
https://doaj.org/article/05b9c95d43ff4b7685d5e2eafa6bc283
Publikováno v:
McNaughton, K G, Clement, R J & Moncrieff, J B 2007, ' Scaling properties of velocity and temperature spectra above the surface friction layer in a convective atmospheric boundary layer ', Nonlinear Processes in Geophysics, vol. 14, no. 3, pp. 257-271 . https://doi.org/10.5194/npg-14-257-2007
Nonlinear Processes in Geophysics, Vol 14, Iss 3, Pp 257-271 (2007)
Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics, European Geosciences Union (EGU), 2007, 14 (3), pp.257-271
Nonlinear Processes in Geophysics, Vol 14, Iss 3, Pp 257-271 (2007)
Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics, European Geosciences Union (EGU), 2007, 14 (3), pp.257-271
We report velocity and temperature spectra measured at nine levels from 1.42 meters up to 25.7 m over a smooth playa in Western Utah. Data are from highly convective conditions when the magnitude of the Obukhov length (our proxy for the depth of the
Publikováno v:
Journal of Chemical Ecology. 23:1216-1221
Autor:
K. G. McNAUGHTON
Publikováno v:
Plant, Cell and Environment. 17:1061-1068
In nature surfaces are rarely uniform, so terms such as ‘surface’, ‘stomatal’ or ‘canopy’ resistance usually indicate some kind of average over a population of sub-areas, each with its own separate resistance. Questions then arise as to h