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M a c r o c e l l P r e d i c t i o n M o d e l s - P a r t 2 : P o i n t - t o - P o i n t M o d e l s 121
3.1.4.2 Terrain Averaging
When a terrain-averaging program is turned on, the Lee model uses a simple running
average by averaging the elevations from three points, the current local point, the pre
ceding point, and the succeeding point to find a new elevation at the current local point.
For example, when the averaging scope is set to 5 points, the new elevation for any
given point on the radial is obtained by averaging the current elevation with the 2 pre
vious points and 2 succeeding points along the radial.
For those points where only fewer than 3 or 5 points can be averaged (such as the
last point on a radial), the extrapolate elevations are used for those points.
3 . 1 . 4.3 Effective Earth Curvature12·13
When the distance is greater than 10 miles, we may consider the effect of earth curva
ture. Terrain elevation values can be adjusted with an offset value to compensate for the
horizon effect caused by the earth's curvature. This offset represents a reduction in
elevation at the point of the mobile, which increases with distance from the base station.
When the earth curvature offset is used, a parameter known as the K factor can be
specified to represent the earth's radius. This parameter is used to adjust the earth cur
vature offset to compensate for the slight curvature of the signal path.
The earth curvature offset can be turned on or off based on a specified value for the
K factor, as described below.
3.1.4.3.1 Earth Curvature Offset The earth curvature offset value is the difference between
a straight line drawn from the site elevation point to a point along the radial as compared
with the curve of the earth through these same points, as illustrated in Fig. 3.1.4.3.1.
A formula for the earth curvature offset can be derived as follows:
1 . Consider a mobile elevation point is at a distance (D) in meters from the site
elevation and assume the earth's radius (R) to be 6,370,997 m.
2. The angular distance from the site to a point is given by
. D
ang e = (3 1 . 4.3.1)
.
1 a rc sm
R
3. The dip below the horizon is given by
.
dip = (1.0 - cos( angle)) x R (3 1 .4.3.2)
3.1.4.3.2 K Factor When the earth curvature option in the prediction model is turned
on, a parameter known as the K factor can be specified to adjust the calculated earth
curvature offset. The K factor represents a proportion of the actual radius of the earth.
1
The Lee model uses a default value of . 33:
2
Offset = 2D /3K (3.1.4.3.5)
Any value of K factor larger than 1 assumes that the radius of the earth is larger than
the actual one, thus resulting in a smaller earth curvature offset. Because the signal path
is somewhat curved rather than straight, the signal horizon is lower than would be
represented by drawing a straight line from the transmitter to the mobile. Thus, the
earth curvature offset should be less than that calculated by using the actual radius of
the earth, and use of K factor values larger than 1 is recommended.