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90 Living Energies EXOSPHERE: The outermost layer of the Earth's atmosphere extending from about 400km- 500km above the Earth's surface, where terrestrial gravitation is too weak an effect to prevent the escape of uncharged particles. THERMOSPHERE: An atmospheric layer lying between the mesosphere and the exosphere, reaching an altitude of about 400km, where the temperature is over 1000°C. [Is this thermal or kinetic? - CC] IONOPAUSE: IONOSPHERE: F-REGION: The transitional zone in the atmosphere between the ionosphere and the exosphere about 644km (400 miles) from the Earth's surface. A region of the Earth's atmosphere extending from about 60km to 1000km above the Earth's surface in which there is a high concentration of free electrons formed as a result of ionising radiation entering the atmosphere from space. 150km-1000km. Highest proportion of free electrons and most useful for long- range radio transmissions, also called the Appleton Layer. [+4°C stratum at about 175 km-CC] 90km-150km. Reflects radio waves of medium wavelength, also called the E-REGION: Heaviside Layer. [+4°C stratum at about 85km - CC] D-REGION: MESOPAUSE: MESOSPHERE: STRATOPAUSE: STRATOSPHERE: TROPOPAUSE: TROPOSPHERE: 60km-90km. Lowest region of the ionosphere - Low concentration of free electrons and reflects low-frequency radio waves. [+4°C stratum at about 72km - CC] The zone of minimum temperature between the mesosphere and the thermosphere. The atmospheric layer lying between the stratosphere and the thermosphere characterised by a rapid increase in temperature with height. The atmospheric zone immediately above the stratosphere marked by a temperature maximum of +10°C between altitudes of 48km and 53km. The transitional zone of maximum temperature between the stratosphere and the mesosphere. The atmospheric layer lying between the troposphere and the mesosphere in which the temperature generally increases with height. The atmospheric zone immediately above the tropopause, including the Ozone layer. The plane of discontinuity between the troposphere and the stratosphere characterised by a sharp change in the lapse rate4 and varying in altitude from about 18km (11 miles) above the equator to 6km (4 miles) above the Poles. The lowest atmospheric layer about 18km thick at the equator and 6km thick at the Poles in which air temperature decreases with height at about 6.5°C/km. Most meteorological phenomena occur in this layer. The innermost zone of the Earth's atmosphere extending from the surface to the tropopause. Fig. 6.1 The Structure of the AtmospherePDF Image | Viktor Schauberger Work Explained
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