The Stable Atmospheric Boundary Layer over an Antarctic ice Sheet

被引:0
作者
Dörthe Handorf
Thomas Foken
Christoph Kottmeier
机构
[1] Alfred Wegener Institute for Marine and Polar Research,Dept. of Micrometeorology
[2] Research Department,Institute of Meteorology and Climate Research
[3] Potsdam,undefined
[4] University of Bayreuth,undefined
[5] University of Karlsruhe,undefined
来源
Boundary-Layer Meteorology | 1999年 / 91卷
关键词
Stable boundary layer; Boundary-layer height; Universal functions; Similarity theory;
D O I
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中图分类号
学科分类号
摘要
Turbulence measurements up to 11-m height and longterm profile measurements up to 45-m height performed at the German Neumayer Station in Antarctica are used to investigate different components of turbulence closure schemes of the stable boundary layer. The results confirm the linear relationships for the universal functions of momentum and heat exchange in the stability range z/L < 0.8 ... 1, whereas the local scaling approach should be used above the surface layer. Furthermore, boundary-layer heights below 50 m are frequently observed at this coastal Antarctic site, mainly due to the influence of stability above the boundary layer. It is shown that the inclusion of this stability into parametrization relations is necessary to provide realistic equilibrium heights of the stable boundary layer. Two relations, based on different physical approaches, were successfully applied for the parametrization of the equilibrium height.
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页码:165 / 189
页数:24
相关论文
共 59 条
[1]  
Akima H.(1970)A New Method of Interpolation and Smooth Curve Fitting Based on Local Procedures J. Assoc. Comp. Mach. 17 589-602
[2]  
Andrén A.(1995)The Structure of Stably Stratified Atmospheric Boundary Layers. A Large-Eddy-Simulation Study Quart. J. Roy. Meteorol. Soc. 48 1690-1698
[3]  
Ball F. K.(1956)The Theory of Strong Katabatic Winds Austral. J. Phys. 9 373-386
[4]  
Brost R. A.(1978)A Model Study of the Stably Stratified Planetary Boundary Layer J. Atmos. Sci. 35 1427-1440
[5]  
Wyngaard J. C.(1971)Fluxprofile Relationships in the Atmospheric Surface Layer J. Atmos. Sci. 28 181-189
[6]  
Businger J. A.(1990)Nieuwstadt's Stable Boundary Layer Revisited Quart. J. Roy. Meteorol. Soc. 116 127-158
[7]  
Wyngaard J. C.(1974)A Review of Flux-Profile Relationships Boundary-Layer Meteorol. 7 363-372
[8]  
Izumi Y.(1991)Radiation Fog: A Comparison of Model Simulation with Detailed Observations Mon. Wea. Rev. 119 324-341
[9]  
Bradley E. F.(1905)On the Influence of the Earth's Rotation on Ocean Currents Arkiv. Mat. Astron. Fysik. 2 1-53
[10]  
Derbyshire S. H.(1996)Tools for Quality Assessment of Surface-Based Flux Measurements Agric. For. Meteorol. 78 83-105