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A Theory for Soil Temperature Calculation L N Gutman
On the Determination of the Steady Wind Current in
The Influence of Clouds on the Atmospheric Heat Balance
4 other sections not shown
A.F. Chudnovskii absorption coefficient absorption spectrum Academy of Sciences advective heat influx air temperature albedo approximate assume atmos atmosfere atmospheric layers boundary conditions boundary layer CM CM consider constant coordinate d d d d daily march denote density depth derived determinant E.M. Feigel'son E.S. Kuznetsov earth's surface function Geofiz Geophysical Series Gostekhizdat heat balance heat conductivity In-ta infinite system initial temperature distribution integral equations interval inverse matrix linear algebraic long-wave radiation low absorption coefficient Main Geophysical Observatory matrix mean daily method number in column o o d d obtain the following ocean optical thickness parameters problem quantities radiation flux radiational heat exchange scattering shown snow cover solar radiation solution solved Substituting surface layer Table temperature changes temperature march thermal thickness tion Tr[udy turbulent USSR uuinioo values Volterra integral equation water vapor wind