The effective radiated power of WWJ in the horizontal plane, at the peak value of its daytime azimuth pattern is about 5.5 X that of WJR.
Even so, the distances to the 2.5 mV/m, 0.5 mV/m and 0.15 mV/m groundwave contours are bit less in that direction for Class B WWJ in the daytime than for Class A WJR in that general direction. Probably this is the opposite of what would be expected.
Both groundwave signals travel across paths with virtually the same ground conductivity, M3 values or not.
Factors in this are:
(1) The WJR transmitter site is located somewhat north of the WWJ site, so the propagation path from WJR to those contours is a little shorter in that general direction.
(2) The groundwave propagation losses for WJR on 760 kHz are not as high as for WWJ on 950 kHz. This is reflected in the paper linked below, which charts the relationships between frequency and groundwave field intensity for several values of transmitter power and ground conductivity.
http://www.thebdr.net/articles/rf/xmit/Contours.pdf
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Even so, the distances to the 2.5 mV/m, 0.5 mV/m and 0.15 mV/m groundwave contours are bit less in that direction for Class B WWJ in the daytime than for Class A WJR in that general direction. Probably this is the opposite of what would be expected.
Both groundwave signals travel across paths with virtually the same ground conductivity, M3 values or not.
Factors in this are:
(1) The WJR transmitter site is located somewhat north of the WWJ site, so the propagation path from WJR to those contours is a little shorter in that general direction.
(2) The groundwave propagation losses for WJR on 760 kHz are not as high as for WWJ on 950 kHz. This is reflected in the paper linked below, which charts the relationships between frequency and groundwave field intensity for several values of transmitter power and ground conductivity.
http://www.thebdr.net/articles/rf/xmit/Contours.pdf
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