Katabatic winds: A field case study

Results of a case study of katabatic winds utilizing tethered balloon profiling equipment are presented and discussed. The data are unique in the detail they provide of both vector wind and potential virtual temperature throughout the flow. It is concluded from the data that the one-dimensional models so far proposed in the literature are inappropriate. Direct computation shows that the divergence of radiation responsible for cooling the air is much smaller than the surface radiation flux used in these models. The inadequacy of these models is not due to the underlying assumption of temporal invariance, but rather the implication is that the flow is significantly three dimensional. Use of surface stress as the retarding stress in the dynamical balance is also shown to be erroneous, at least so long as ambient wind does not assist the katabatic flow. The stress between the flow and the ambient air is much more important and this stress is inextricably tied in with the downslope development of the flow which is thus inferred to play a major part in the dynamics of katabatic winds. Katabatic flow is an example of an internal mixing process. The data are shown to suggest a critical gradient Richardson number of about 1/4 for the maintenance of internal mixing above slope flows.

[1]  P. Manins,et al.  A Model of Katabatic Winds , 1979 .

[2]  J. Kondo,et al.  Heat and Momentum Transfers under Strong Stability in the Atmospheric Surface Layer , 1978 .

[3]  E. Carmack,et al.  River‐induced currents in a Fjord Lake , 1978 .

[4]  P. Richards,et al.  Modelling surface turbulent fluxes in stable conditions , 1978 .

[5]  P. Manins,et al.  A self-contained tethered balloon sounding system , 1978 .

[6]  A. Thorpe,et al.  The nocturnal jet , 1977 .

[7]  K. Kitabayashi Wind Tunnel and Field Studies of Stagnant Flow Upstream of a Ridge , 1977 .

[8]  B. C. Ryan A Mathematical Model for Diagnosis and Prediction of Surface Winds in Mountainous Terrain. , 1977 .

[9]  Roland B. Stull,et al.  The Energetics of Entrainment Across a Density Interface , 1976 .

[10]  B. Hicks,et al.  Wind profile relationships from the ‘wangara’ experiment , 1976 .

[11]  R. R. Long The influence of shear on mixing across density interfaces , 1975, Journal of Fluid Mechanics.

[12]  F. Hall,et al.  Convective Plumes in the Planetary Boundary Layer, Investigated with an Acoustic Echo Sounder , 1975 .

[13]  G. Wendler,et al.  Some observations of the local wind regime on an alaskan arctic glacier , 1974 .

[14]  J. Turner,et al.  Buoyancy Effects in Fluids: Subject Index , 1973 .

[15]  S. Arya The critical condition for the maintenance of turbulence in stratified flows , 1972 .

[16]  R. H. Clarke,et al.  The Morning Glory: An Atmospheric Hydraulic Jump , 1972 .

[17]  W. Brutsaert Radiation, evaporation and the maintenance of turbulence under stable conditions in the lower atmosphere , 1972 .

[18]  A. Hočevar,et al.  Night drainage winds , 1971 .

[19]  E. F. Bradley,et al.  Flux-Profile Relationships in the Atmospheric Surface Layer , 1971 .

[20]  E. K. Webb,et al.  The temperature fluctuations in stable stratification , 1970 .

[21]  D. O. Staley,et al.  Flux Emissivity Tables for Water Vapor, Carbon Dioxide and Ozone , 1970 .

[22]  K. Buettner,et al.  Valley winds in the mount Rainier area , 1965 .

[23]  D. O. Staley Radiative cooling in the vicinity of inversions and the tropopause , 1965 .

[24]  J. P. Funk Radiative flux divergence in radiation fog , 1962 .

[25]  J. Turner,et al.  Turbulent entrainment in stratified flows , 1959, Journal of Fluid Mechanics.

[26]  A. Blackadar Boundary Layer Wind Maxima and Their Significance for the Growth of Nocturnal Inversions , 1957 .

[27]  F. Ball The theory of strong katabatic winds , 1956 .

[28]  T. A. Gleeson EFFECTS OF VARIOUS FACTORS ON VALLEY WINDS , 1953 .

[29]  R. G. Fleagle A THEORY OF AIR DRAINAGE , 1950 .

[30]  R. H. Clarke,et al.  Observational studies in the atmospheric boundary layer , 1970 .