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Bernese GPS Software Version 5.0 - Bernese GNSS Software

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2. Fundamentals<br />

where aROCK is the acceleration due to the Rock4 (Block I satellites) and Rock42 (Block<br />

II satellites) models for the radiation pressure [Fliegel et al., 1992], and<br />

where<br />

aD = (aD0 + aDC · cos u + aDS · sin u) · eD = D(u) · eD<br />

aY = (aY 0 + aY C · cos u + aY S · sin u) · eY = Y (u) · eY<br />

aX = (aX0 + aXC · cos u + aXS · sin u) · eX = X(u) · eX<br />

(2.10)<br />

aD0, aDC, aDS, aY 0, aY C, aY S, aX0, aXC, and aXS are the nine parameters of the radiation<br />

pressure model of the <strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> <strong>Version</strong> <strong>5.0</strong> ,<br />

eD is the unit vector satellite-to-sun,<br />

eY = eD × r<br />

is the unit vector along the spacecraft’s solar-panel axis assuming nominal<br />

|eD × r|<br />

satellite attitude (see Figure 2.2),<br />

eX = eY × eD completes a right-handed orthogonal system of unit vectors,<br />

D(u), Y (u), and X(u) are the total accelerations due to radiation pressure (on top of the<br />

Rock4/42-models) in the directions eD, eY , and eX, and<br />

u is the argument of latitude at time t for the satellite considered.<br />

For <strong>GPS</strong> satellites the ROCK4/42 model, version T (including thermal re-radiation, also<br />

called T10 and T20) is used at CODE. The a priori model is automatically scaled by<br />

the factor r 2 0 /r2 , where r0 is the Astronomical Unit (AU), and r is the actual distance<br />

between Sun and spacecraft. In order to compute the actual accelerations acting on the<br />

satellite, ROCK models require the satellite mass. The satellite masses are given (together<br />

with other satellite specific information like the antenna phase center eccentricity) in the<br />

satellite information file (e.g., ${X}/GEN/SATELLIT.I05, see Section 22.4.5). Alternatively<br />

to the ROCK4/42 model the model developed by [Springer et al., 1999] may be used as<br />

a priori radiation pressure model (see Section 15). For GLONASS satellites no radiation<br />

pressure model is available and, therefore, no a priori model is applied.<br />

The acceleration due to the solar radiation pressure is switched off when the satellite is in<br />

the Earth’s shadow and scaled according to the fraction of the solar disk not covered by the<br />

Moon during lunar partial eclipses that regularly occur during New Moon.<br />

In summary, in <strong>Version</strong> <strong>5.0</strong> of the <strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> each satellite arc is characterized<br />

by six osculating elements and by up to nine dynamical parameters as defined above. The<br />

parameterization of the a priori orbits is defined in program ORBGEN (see Section 5.4.2).<br />

2.2.2.4 Pseudo-Stochastic Orbit Parameterization<br />

Whereas most users of the <strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> only have to deal with the n = 6 + np ≤ 15<br />

deterministic orbit parameters discussed in the previous section, the advanced user working<br />

on orbit determination might also wish to parameterize the orbits additionally with<br />

so-called pseudo-stochastic parameters, characterizing instantaneous velocity changes at<br />

user-determined epochs in user-determined directions. The attribute stochastic is justified<br />

Page 32 AIUB

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