Science: v.1-v.219Moses King, 1966 |
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Page 1023
... 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 radio propa- gation at ...
... 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 radio propa- gation at ...
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 1212
... electron and the magnitude of the unit of electric charge , appear in the theory as arbitrary parameters whose value must be determined by experi- ment . One would hope , in a complete theory , that these would be predicted also . The ...
... electron and the magnitude of the unit of electric charge , appear in the theory as arbitrary parameters whose value must be determined by experi- ment . One would hope , in a complete theory , that these would be predicted also . The ...
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