Heat balance of the Earth

Results of improved calculations of the heat balance components of Earth's surface are reported for yearly average conditions. The technique used to determine the heat-balance components from land- and sea-based actinometric observations as well as from satellite data on the radiation balance of the Earth-atmosphere system is described, with special attention given to short-wavelength solar radiation on the continents, effective radiation from the land surface, the radiation balance of the ocean surface, heat expended by both evaporation from the ocean surface, and turbulent heat transfer between the ocean surface and the atmosphere. World maps of heat-balance components show yearly average values of total radiation, radiation balance, heat expended by evaporation, the turbulent heat flow between Earth's surface and atmosphere, and heat transfer between the ocean surface and underlying waters. The global surface heat balance is estimated along with global values of the various components and the heat-balance components for different latitude zones

Study of natural magnetization titanomagnetite ores Gusevogorskoye deposit (from measurements in boreholes)

The work shows the results of measurements magnetization (natural complete, natural residual and induced magnetization, inclination of angles complete and residual magnetization, ratio Koenigsberger) titanomagnetite ores Gusevogorskoye deposit in natural situ. The data was received by results of a three-component borehole magnetometer, measurement in explosive holes in Kachkanar. It is concluded that the observed changes in the natural residual magnetization indicate the formation of titanomagnetite ores in different thermodynamic areas as a result of subsequent geological processes that led to the disintegration of solid solutions. The main magnetic phase of these deposits were quite similar in composition and magnetic structure