Titlebook: Boundary Layer Studies and Applications; A Special Issue of B R. E. Munn Book 1989 Kluwer Academic Publishers 1989 Meteorology.Scale.Wind s

Stenosis

書目名稱Boundary Layer Studies and Applications影響因子(影響力)




書目名稱Boundary Layer Studies and Applications影響因子(影響力)學(xué)科排名




書目名稱Boundary Layer Studies and Applications網(wǎng)絡(luò)公開度




書目名稱Boundary Layer Studies and Applications網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Boundary Layer Studies and Applications被引頻次




書目名稱Boundary Layer Studies and Applications被引頻次學(xué)科排名




書目名稱Boundary Layer Studies and Applications年度引用




書目名稱Boundary Layer Studies and Applications年度引用學(xué)科排名




書目名稱Boundary Layer Studies and Applications讀者反饋




書目名稱Boundary Layer Studies and Applications讀者反饋學(xué)科排名

秘傳

An Evaluation of Aircraft Flux Measurements of CO2, Water Vapor and Sensible Heat,x. Cospectral analyses showed no significant high frequency losses for the data from flight levels of 25 and 50 m, but an underestimation of approximately 10% resulted at 10 m. Flight direction with respect to wind direction was relatively unimportant at 10 and 25 m but some effects were observed at

肌肉

Spectra of Surface Wind Speed and Air Temperature over the Ocean in the Mesoscale Frequency Range in buoys. Significant mesoscale peaks in spectra appear in relatively strong winds and unstable or near-neutral atmospheric conditions, and none in stable atmospheric conditions. A criterion of wind speed and atmospheric stability is found for the mesoscale spectral peak appearance.

Outshine

The Spectral Velocity Tensor for Homogeneous Boundary-Layer Turbulence,n the transition domain from the inertial subrange towards lower wave numbers. When the three sets of parameters are the same, the three spectra correspond to isotropic turbulence and they are all interrelated and related to the energy spectrum. We show how it is possible to obtain these spectral fo

Abutment

Spatial Correlation Functions of Surface-Layer Atmospheric Turbulence in Neutral Stratification,turbulence. In Section 3 it is shown that the correlation equations of Section 2 agree satisfactorily with some recent measurements of the longitudinal correlation functions in the range of distances from 3 m to 100 m. Some measurements of the lateral correlation functions of atmospheric turbulence

奴才

烤架

弄皺

motor-unit

electrolyte