Analysis of the unsteadiness of the hemispherical temperature gradient of the atmosphere

Details Analysis of the unsteadiness of the hemispherical temperature gradient of the atmosphere Analysis of the unsteadiness of the hemispherical temperature gradient of the atmosphere

May 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981fizao..17..451m&link_type=abstract

Akademiia Nauk SSSR, Izvestiia, Fizika Atmosfery i Okeana, vol. 17, May 1981, p. 451-463. In Russian.

Other

Anomalous Temperature Zones, Atmospheric Circulation, Atmospheric Heating, Atmospheric Temperature, Periodic Variations, Temperature Gradients, Air Water Interactions, Atmospheric Energy Sources, Baroclinity, Heat Transfer, Hydrodynamic Equations, Hydrothermal Systems

Scientific paper

An analysis is presented of the effect of unsteady nonadiabatic heat sources (anomalies in deviations from the annual cycle) on anomalies of the planetary baroclinity of the atmosphere. The analysis employs the basic and adjoint hydrothermodynamic equations of the atmosphere, and both direct and inverse methods are used. It is shown that the adjoint equations can be effectively used to analyze unsteady atmospheric processes with a characteristic time of the order of one week and a horizontal scale equal to a continent.

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