Seite - 61 - in Contributions to GRACE Gravity Field Recovery - Improvements in Dynamic Orbit Integration, Stochastic Modelling of the Antenna Offset Correction, and Co-Estimation of Satellite Orientations
Bild der Seite - 61 -
Text der Seite - 61 -
6.5 Fit of Stochastic Model
To compute an optimal least squares solution of the daily and monthly Stokes coef-
ficients, the stochastic characteristics of the observation data must be considered. In
ITSG-Grace2016, four observation groups are present: the hl-SST POD observations
for both GRACE-A and GRACE-B, the ll-SST KBR observations, and the pseudo-
observations used to constrain the daily Stokes coefficients. Each observation group
has associated
residuals
∆lpod,A
∆lpod,B
∆lsst
lgpm
=Ax+
epod,A
epod,B
esst
egpm
(6.5.1)
which are distributed according to their respective covariance
matrices
epod,A
epod,B
esst
egpm
∼N
0,
ΣpodA 0 0 0
0 ΣpodB 0 0
0 0 Σsst 0
0 0 0 Σgpm
. (6.5.2)
In ITSG-Grace2016, it is assumed that the observation groups are not cross-correlated.
Only the structure of the covariance matrix due to the geophysical modelQgpm is
known a priori, the remaining covariance matrices are determined in ITSG-Grace2016
through variance component estimation.
Thestochasticmodel isre-estimatedforeachgeneratedmonthlysolutioninamulti-step
process. To this end, a GRACE monthly gravity field solution of decreased degree and
order of only 60 is computed while iteratively adjusting the weights of the observation
groups and refining the covariance structure of each observation group. The gravity
field solution is computed at a reduced fidelity to speed up the time-consuming
iteration of the computation.
6.5.1 Toeplitz Covariance Structure
The noise of the POD and KBR observations is assumed to be the result of a wide-sense
stationary process, meaning that the autocovariance function of the noise signal does
not vary with time, or in the case of ITSG-Grace2016, within one month. Such a process
can be fully described by its autocovariance function (Etten, 2006)
Cxx(t1,t2)=Cxx(t2− t1)=Cxx(∆t) . (6.5.3)
This covariance function is estimated once per observation type and month. The re-
estimation for every month implies that the estimated noise model is stationary for
6.5 Fit of Stochastic Model 61
Contributions to GRACE Gravity Field Recovery
Improvements in Dynamic Orbit Integration, Stochastic Modelling of the Antenna Offset Correction, and Co-Estimation of Satellite Orientations
- Titel
- Contributions to GRACE Gravity Field Recovery
- Untertitel
- Improvements in Dynamic Orbit Integration, Stochastic Modelling of the Antenna Offset Correction, and Co-Estimation of Satellite Orientations
- Autor
- Matthias Ellmerr
- Verlag
- Verlag der Technischen Universität Graz
- Ort
- Graz
- Datum
- 2018
- Sprache
- englisch
- Lizenz
- CC BY 4.0
- ISBN
- 978-3-85125-646-8
- Abmessungen
- 21.0 x 29.7 cm
- Seiten
- 185
- Schlagwörter
- Geodäsie, Gravitation, Geodesy, Physics, Physik
- Kategorien
- Naturwissenschaften Physik
- Technik