Science: v.1-v.219Moses King, 1966 |
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Page 1023
... Electron Density The natural electron density in the daytime ionospheric " E layer " at 100 km altitude is about 105 electrons per cubic centimeter , decaying at night to below 104. The daytime layer is re- sponsible for over - horizon ...
... Electron Density The natural electron density in the daytime ionospheric " E layer " at 100 km altitude is about 105 electrons per cubic centimeter , decaying at night to below 104. The daytime layer is re- sponsible for over - horizon ...
Page 1024
... electron inventory . These clouds were often lost because they drifted out of the antenna patterns rather than because of decay to back- ground electron density . At altitudes below 95 km , oxidation of cesium vapor , as well as ...
... electron inventory . These clouds were often lost because they drifted out of the antenna patterns rather than because of decay to back- ground electron density . At altitudes below 95 km , oxidation of cesium vapor , as well as ...
Page 1211
... electron —that is , enough energy to be equiv- alent to the mass of one electron- the process does not take place . But when energy equivalent to two elec- trons is available , an electron - positron pair is created . What causes the ...
... electron —that is , enough energy to be equiv- alent to the mass of one electron- the process does not take place . But when energy equivalent to two elec- trons is available , an electron - positron pair is created . What causes the ...
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