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Journal ArticleDOI

Sensitivity analysis of the equations for a convective mixed layer

TLDR
In this paper, the authors analyzed the sensitivity of the solutions of the model equations to variations in the entrainment formulation and in the initial and boundary conditions, and showed that the initial conditions for the mixed-layer height (h) and potential temperature (m) quickly lose their influence.
Abstract
Jump or slab models are frequently used to calculate the depth of the convectively mixed layer and its potential temperature during the course of a clear day. Much attention has been paid theoretically to the parameterization of the budget for turbulent kinetic energy that is required in these models. However, for practical applications the sensitivity of the solutions of the model equations to variations in the entrainment formulation and in the initial and boundary conditions is also very important. We analyzed this sensitivity on the basis of an analytical solution for the model which uses the well-known constant heat flux ratio. The initial conditions for the mixed-layer height (h) and potential temperature (θ m ) quickly lose their influence. Only the initial temperature deficit is important. The mixed-layer temperature at noon on convective days is insensitive to the entrainment coefficient c. It is governed by the integral of the heat input and by the stable lapse rate. A change in c from 0.2 to 0.5 leads to a variation of 20% in h. This is not very much considering the accuracy in the determination of h from actual observations.

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Citations
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Journal ArticleDOI

Review and intercomparison of operational methods for the determination of the mixing height

TL;DR: In this paper, the authors present a review of the literature on the analysis of profile measurements and the use of parameterisations and simple models, and suggest for the preprocessor development and for future research activities.
Journal ArticleDOI

Models and observations of the growth of the atmospheric boundary layer

TL;DR: In this article, the evolution of the mixed layer during a clear day can be described with a slab model and the model equations have to be closed by a parameterization of the turbulent kinetic energy budget.
Book ChapterDOI

Atmospheric boundary layer research at Cabauw.

TL;DR: In this paper, a 213 m high mast specifically built for meteorological research has been operational since 1973 at Cabauw, The Netherlands, and its site, construction, instrumentation and observation programs are reviewed.
Journal ArticleDOI

Entrainment Effects in the Well-Mixed Atmospheric Boundary Layer

TL;DR: In this paper, the structure and evolution of a cloud-free atmospheric boundary layer (ABL) during daytime over land, starting from a shallow ABL at sunrise and developing into a deep ABL with strong convection in the afternoon, is discussed.
References
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Journal ArticleDOI

The Energetics of Entrainment Across a Density Interface

TL;DR: In this article, a theory of the fluid entrainment rate into a turbulent, mixed layer across a horizontal density interface is presented by integrating the turbulent kinetic energy equation over the depth of the mixed layer and assuming that turbulence dissipation rates are proportional to production rates.
Journal ArticleDOI

Basic entrainment equations for the atmospheric boundary layer

TL;DR: In this paper, the authors reviewed the parameterization of penetrative convection and other cases of turbulent entrainment by the atmospheric boundary layer, and the conservation equations for a one-layer model of entrainments are straightforward; all modeling problems arise in the context of the parameterisation of various terms in the budget of turbulent kinetic energy.
Journal ArticleDOI

On the modelling of mixed layers and entrainment in cumulus cloud

TL;DR: In this article, a boundary-layer model incorporating an eddy diffusivity for turbulent transports is presented to predict the appropriate behaviour for mixed layers produced by surface shear, free convection and mechanical mixing.