Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 448878
Title The Onset of the Very Stable Boundary Layer
Author(s) Wiel, B.J.H. van de; Moene, A.F.; Jonker, H.J.J.; Baas, P.; Basu, S.; Donda, J.; Sun, J.; Holtslag, A.A.M.
Event EGU General Assembly 2013, Vienna, 2013-04-07/2013-04-12
Department(s) Meteorology and Air Quality
WIMEK
Publication type Abstract in scientific journal or proceedings
Publication year 2013
Abstract Here, the mechanism behind the collapse of turbulence in the evening is investigated as a precursor to the onset of the very stable boundary layer. A cooled, pressure-driven flow is investigated by means of a local similarity model. Simulations reveal a temporary collapse of turbulence whenever the surface heat extraction, expressed in its nondimensional form h/L, exceeds a critical value. As any temporary reduction of turbulent friction is followed by flow acceleration, the long-term state is unconditionally turbulent. In contrast, the temporary cessation of turbulence, which may actually last for several hours in the nocturnal boundary layer, can be understood from the fact that the time scale for boundary layer diffusion is much smaller than the time-scale for flow acceleration. This limits the available momentum that can be used for downward heat transport. In case the surface heat extraction exceeds the so-called maximum sustainable heat flux (MSHF), the near-surface inversion rapidly increases. Turbulent activity is largely suppressed by the intense density stratification which supports the emergence of a different, calmer boundary layer regime. Finally, results are translated into a practical model to predict the minimum wind speed for sustained turbulence in the atmosphere. It is shown that under clear sky conditions 5 m/s is the typical geostrophic wind limit for Cabauw, below which continuous turbulence cannot be sustained. Below this threshold therefore the emergence of the very stable nocturnal boundary regime is foreseen.
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