11.4.5  Time Transfer Using GPS
Time transfers (clock comparisons) may be made in a number of ways using the GPS
satellites.  The time dissemination process described in paragraph 11.4.4 is a "passive"
method, in which the user acquires an accurate time reference without having to
transmit timing signals or data.  Other ways that can provide more accu rate
comparisons are described in this section.
11.4.5.1  Coordinated Simultaneous
 View Time Transfer
In this method, a pair of stations simultaneously observes the same satellite(s); then
(through some communications medium) they exchange readings of their local clock
time against the time disseminated by GPS.  The difference between these readings is
quite accurately the difference between the stations  clocks.  The satellite clock is
primarily a transfer clock and does not directly affect the time transfer accuracy.  This
method might be used where the user clocks are required to maintain time or frequency
agreement more precisely than UTC can be disseminated through GPS.  The method
works particularly well when the participating clocks are located reasonably close
together (within some hundreds of kilometers).  The method can also substan tially
reduce the effects of S/A on time transfers made with the C/A code, because both
ephemeris and ionospheric effects are reduced. Unless the time transfer is made with
USNO or a UTC(USNO) traceable reference, the result is relative rather than absolute
time accuracy.
11.4.5.2  Coordinated Simultaneous
 View Time Transfer with USNO
USNO uses a coordinated simultaneous  view method as shown in Figure 11 5, to
provide more accurate UTC(USNO) to certain Pre cise Time Stations within
simultaneous view range.  Both USNO and the distant observer track the same GPS
satellite(s), derive UTC (USNO) from the satellite s NAV msg and pseudorange
measurements, and compare this time with the time maintained by t heir local atomic
clocks.  USNO compares UTC (USNO) derived from the GPS satellites with the USNO
Master Clock.  Thus, USNO can deter mine the Control Segment and Satellite   induced
errors that the observer will have in his GPS  derived UTC(USNO).  The distant
observer can then correct his GPS derived UTC (USNO) with correc tions received from
USNO via a data link.  Now the distant observer can correct his clock very accurately to
serve as a local reference traceable to UTC (USNO). The time accuracies that can be
obtained by this method are shown in Table 11 1.  The Table 11  1 values are valid for
time transfer using C/A code only when SA is switched off. Smoothing of the time
measurements brings the error down to what can be expected for a P code receiver.
The errors due to ephemeris uncertainties and ionospheric delay usually cancel out of
if the two receivers are close to each other.  This is because they have nearly the same
line of sight to the satellites, and the signals travel through the same part of the iono  
sphere.  In some cases where the two receivers are close to each other, the use of both
L1 and L2 to compensate for iono spheric delay will be less accurate than not correcting
for ionospheric delay at all.  This is due to the fact that dual frequency com pensation
for ionospheric delay is not perfect, and use of the ionospheric delay broad cast by the
satellite by both parties produces more accurate results.  For most cases where
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