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ExtraClassSylalbus2009jan-AD7FO

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Rev 2.02<br />

E3C01<br />

Auroral activity causes radio communication of CW signals have a fluttery tone.<br />

E3C02<br />

The cause of auroral activity is the emission of charged particles from the sun.<br />

E3C03<br />

Auroral activity in the ionosphere occurs at E-region height.<br />

E3C04<br />

The CW emission mode is best for auroral propagation.<br />

E3C05<br />

Selective fading is caused by phase differences in the received signal caused by different paths.<br />

E3C06<br />

VHF/UHF radio-path horizon distance exceeds the geometric horizon by approximately 15% of the distance.<br />

E3C07<br />

The radiation pattern of a 3-element, horizontally polarized beam antenna will vary with height above ground. The<br />

main lobe takeoff angle will decrease with increasing height.<br />

E3C08<br />

The name of the high-angle wave in HF propagation that travels for some distance within the F2 region is the<br />

Pedersen ray.<br />

E3C09<br />

Tropospheric ducting is usually responsible for propagating VHF signals over 500 miles.<br />

E3C10<br />

The performance of a horizontally polarized antenna mounted on the side of a hill when compared with the same<br />

antenna mounted on flat ground will have a main lobe takeoff angle that decreases in the downhill direction.<br />

E3C11<br />

From within the contiguous 48 states, an antenna should be pointed approximately north to take maximum<br />

advantage of auroral propagation.<br />

E3C12<br />

As the frequency of a signal is increased, its ground wave propagation decreases.<br />

E3C13<br />

Most ground-wave propagation has a Vertical polarization.<br />

E3C14<br />

Because VHF and UHF radio waves may be bent, the radio-path horizon distance can exceed the geometric<br />

horizon (by about 15%).<br />

Jack Tiley <strong>AD7FO</strong> Page 27 3/15/2009

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