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GENERAL INTRODUCTION pages 3 to
Atmospheric Turbulence pages 420463 with height 1231 The surface resistance and
Literature cited in chapter 6 195
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a-curves absorption acceleration adiabatic aerogram aerological air particles albedo ascendent ascent curve assumed atmosphere axis Bjerknes circles of latitude circulation cloud co-ordinates component computed condensation considered const constant cooling corresponding denote density derivative determined diagram differential direction divergence dx dy dy dz dynamic height earth equal equation equilibrium equiscalar curves Eulerian method expression figure fluid formula geometric given graphical heat heat conduction horizontal humidity hypsography integral introduced isallobaric isentropic surface isobaric isobaric surfaces isohypses isothermal kinematic lapse rate latitude layer mass means Meteor meteorology method motion normal oscillation positive potential temperature practical pressure radiative represented rotation saturation scalar scalar fields short-wave radiation solar solenoids streamlines surface of discontinuity tephigram theorem thermodynamic tion trajectories troposphere tube unstable Vaisala values variables variation vector bands vector field vector lines vertical virtual temperature vortex vorticity water vapor wave lengths