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Experimental studies of entrainment at the top of the dry atmospheric boundary layer

Entrainment, the dynamical incorporation of free air into the boundary layer, is important because it affects the temperature and moisture profiles of the boundary layer. Weather forecast models require a parameterization of entrainment so as to more accurately predict cloud formation at the top of the boundary layer; a process sensitive to small changes in relative humidity. Using a tethered-balloon based observing platform with multiple turbulence probes, observations of a convective planetary boundary layer were made to investigate the process of entrainment at the boundary layer's interface with the free atmosphere. Observations were taken throughout the boundary layer at a vertical resolution of about 100rn, enabling two-dimensional scalar fields to be constructed. Measurements made in situ within the entrainment zone were used to calculate the entrainment flux. By applying a filtering technique it was discovered that 50% of the entrainment flux could be attributed to processes occurring on scales larger than the boundary layer depth, Zi. This emphasised the importance of large-scale motions, e.g. thermals, to entrainment. At the other end of the scale, 20% of the entrainment flux was due to processes occurring on scales < zi/4. Hence, small-scale local mixing processes are also relevant to entrainment. Conditional sampling analysis showed that within the upper part of the entrainment zone, over 80% of the entrainment flux is carried by up draughts. The observations provide evidence for two previously postulated mechanisms for entrainment. Specific engulfment episodes are presented. These support recently reported Large-Eddy Simulation work that has resolved engulfment's within a model. Also observed is an instance of an upwelling thermal impinging on and distorting the inversion layer. This interaction results in a local reduction in stability across the inversion layer, allowing entrainment to occur as a result of wave-breaking.

Identiferoai:union.ndltd.org:bl.uk/oai:ethos.bl.uk:604311
Date January 1999
CreatorsClaxton, Bernard M.
PublisherUniversity of Manchester
Source SetsEthos UK
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation

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