Abstract: A solution is given, in the form of influence functions, for the forced geostrophic response of the atmosphere to the combined effects of zonal asymmetries in (i) the lower boundary orography and (ii) the mean, ...

Abstract: A general solution is obtained for forced, stationary, quasi-geostrophic perturbations in an atmosphere having the main zonal-average characteristics of the winter troposphere and stratosphere. Special solutions along 45° ...

Abstract: No abstract available.

Abstract: Not available

Abstract: The results of computations of the spectrum of the eddy kinetic energy, the angular momentum transport, and the transfer of kinetic energy between the eddies and the mean motion, for the month of January 1949, are presented. ...

Abstract: The Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set ...

Abstract: A simplified version of a previously described dynamical model governing global ice mass, atmospheric carbon dioxide, and mean ocean temperature (that may also be a proxy for some other CO2?controlling oceanic variable, ...

Abstract: Because of the small net rates of energy flow involved in very long-term changes in ice mass (10?1 W m?2) it will be impossible to proceed in a purely deductive manner to develop a theory for these changes. An inductive ...

Abstract: Cross sections of the mean meridional wind for winter and summer along five latitudes (15°, 30°, 45°, 60° and 75°N) are presented, and their salient features described.

Abstract: No abstract available.