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J. J. Cramer,P. Vilks,J. P. A. Larocqueeast implicitly, that the unavoidable observation errors are exclusively stochastic with zero expectation. The corresponding variance-covariance matrix (vcm) of the estimated parameters is then computed from the observations’ vcm just by means of variance propagation. However, the complete error bud

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Jatinder Singh,Dhananjay Suresh Gaikwadastic lithosphere and the low viscosity of the asthenosphere below Iceland, the ablation resulted in a retarded land uplift of about 3–8 mm/a in the vicinity of the ice cap. This is confirmed by GPS campaigns carried out south of the ice cap in 1992 and 1996 (Sj?berg et al, 1999). Furthermore, a rel

Apraxia

https://doi.org/10.1007/978-981-97-2405-5s of two satellites co-orbiting in a nearly polar orbit, at approximately 300–500 km altitude, separated by 100–500 km along track. The satellites are to launch in 2001 with a lifetime of approximately 5 years. Primary measurements are the range change between the two satellites using a dual one-way