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Volume 9, issue 2
Earth Syst. Sci. Data, 9, 833–848, 2017
https://doi.org/10.5194/essd-9-833-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Syst. Sci. Data, 9, 833–848, 2017
https://doi.org/10.5194/essd-9-833-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Review article 17 Nov 2017

Review article | 17 Nov 2017

Instrument data simulations for GRACE Follow-on: observation and noise models

Neda Darbeheshti et al.

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Cited articles

Bandikova, T., Flury, J., and Ko, U.: Characteristics and accuracies of the GRACE inter-satellite pointing, Adv. Space Res., 50, 123–135, 2012.
Case, K., Kruizinga, G., and Wu, S.: GRACE level 1B data product user handbook, JPL Publication D-22027, 2002.
Flechtner, F., Neumayer, K.-H., Dahle, C., Dobslaw, H., Fagiolini, E., Raimondo, J.-C., and Güntner, A.: What Can be Expected from the GRACE-FO Laser Ranging Interferometer for Earth Science Applications?, Surv. Geophys., 37, 453–470, https://doi.org/10.1007/s10712-015-9338-y, 2016.
Franklin, J. N.: Numerical simulation of stationary and non-stationary gaussian random processes, SIAM Review, 7, 68–80, 1965.
Gath, P.: Integration und Test der GRACE Follow-On Satelliten, Tech. Rep. 420305, Deutscher Luft- und Raumfahrtkongress, 2016.
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Short summary
The Gravity Recovery and Climate Experiment (GRACE) mission has yielded data on the Earth's gravity field to monitor temporal changes for more than 15 years. GRACE Follow-on will be the first satellite mission to use inter-satellite laser interferometry in space to measure the distance variations between two satellites caused by the Earth's global gravitational field. This paper describes the scientific basis and technical approaches used to simulate the GRACE Follow-on instrument data.
The Gravity Recovery and Climate Experiment (GRACE) mission has yielded data on the Earth's...
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