Is the "Earth-ionosphere capacitor" a valid component in the atmospheric global electric circuit?

被引:30
作者
Haldoupis, Christos [1 ]
Rycroft, Michael [2 ]
Williams, Earle [3 ]
Price, Colin [4 ]
机构
[1] Univ Crete, Dept Phys, Iraklion, Greece
[2] CAESAR Consultancy, 35 Millington Rd, Cambridge, England
[3] MIT, Parsons Lab, 77 Massachusetts Ave, Cambridge, MA 02139 USA
[4] Tel Aviv Univ, Dept Geosci, Porter Sch Environm Sci, Ramat Aviv, Israel
关键词
BALLOON OBSERVATIONS; SEASONAL-VARIATIONS; SOUTH-POLE; CONDUCTIVITY; FIELD; THUNDERSTORMS;
D O I
10.1016/j.jastp.2017.08.012
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper examines whether the Earth-ionosphere capacitor (EIC) model is correct, by comparing observed atmospheric electrical properties with those expected for a spherical capacitor, as defined in electrostatics. The comparisons suggest that the EIC concept cannot be reconciled with, and hence cannot account for, the observations, particularly the rapid reduction of the atmospheric electric field with height that is measured. This means that the spherical EIC concept is incorrect by being too simplistic; it is thus misleading. The reason for this flawed concept is simple: the model disregards the non-uniform conductivity of the atmosphere which requires the presence of a net positive charge in the lower atmosphere that equals in magnitude the Earth's negative charge. This positive charge shields the action of the Earth's negative charge from polarizing the ionosphere positively. Thus, the lower D region ionosphere remains electrically neutral, which makes the EIC concept inappropriate.
引用
收藏
页码:127 / 131
页数:5
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