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Salgsoppgave Tomt Hvit v3.13 - Krogsveen

Salgsoppgave Tomt Hvit v3.13 - Krogsveen

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THE ELECTRICAL STRUCTURE OF THE ATMOSPHERE 25illustrated in Fig. 15 where the average variation in the world-widepotential gradient is compared to the estimated world-wide convectionactivity at different times of day (by GMT). The top graph shows theglobal variations in the electric field measured at sea in the absence oflocal disturbances such as pollution, fog, etc. The top graph seems tocoincide with the lower graph which gives an estimate of the world-wideconvection activity produced by the heat of the sun during a diurnalperiod. The steady convection over oceans, however, is thought tosmooth out the electric field variations as is evident from the topgraph. Before discussing the electrochemical and global thunderstormcircuits as possible generators of the fairweather field, it is necessary toexamine the global leakage current and its implications.2.3 THE AIR TO EARTH CURRENTAs already mentioned, the atmosphere is conducting and the earth'selectric potential or field must cause a current to flow in theatmosphere. Since there is an excess of positive ions residing in theatmosphere and an opposite negative charge bound on the earth'ssurface, charge must flow to earth in the form of a positive ion current.Direct measurements of electric currents in the atmosphere aredifficult if not impossible. Therefore, ion current values at differentaltitudes are almost always computed indirectly from conductivity andelectric field data by the use of Ohm's law. Direct currentmeasurements can be made, however, at ground level by isolating aportion of the earth's surface and measure the charge collected over agiven time. Several methods can be used (Wilson 1906, 1916, Simpson1910, Mühleisen 1953 and Kasemir 1951) but in almost all cases theindirect current gives a value often twice as large as the direct method(Lutz 1939, Israel 1954). Whipple (1932) pointed out that thediscrepancy in currents can be explained by the fact that there is alwaysconvection and eddy diffusion in the atmosphere which will mechanically

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