@ARTICLE{brockmann-etal_14c,
  author = {Brockmann, J. M. and Zehentner, N. and H\"ock, E. and Pail, R. and
	Loth, I. and Mayer-G\"urr, T. and Schuh, W.-D.},
  title = {{EGM\_TIM\_RL05: An Independent Geoid with Centimeter Accuracy Purely
	Based on the GOCE Mission}},
  journal = {Geophysical Research Letters},
  year = {2014},
  volume = {41},
  pages = {8089--8099},
  number = {22},
  abstract = {After more than 4.5 years in orbit, the Gravity field and steady-state
	Ocean Circulation Explorer (GOCE) mission ended with the reentry
	of the satellite on 11 November 2013. This publication serves as
	a reference for the 5th gravity field model based on the time-wise
	approach (EGM_TIM_RL05), a global model only determined from GOCE
	observations. Due to its independence of any other gravity data,
	a consistent and homogeneous set of spherical harmonic coefficients
	up to degree and order 280 (corresponding to spatial resolution of
	71.5 km on ground) is provided including a full covariance matrix
	characterizing the uncertainties of the model. The associated covariance
	matrix realistically describes the model quality. It is the first
	model which is purely based on GOCE including all observations collected
	during the entire mission. The achieved mean global accuracy is 2.4
	cm in terms of geoid heights and 0.7 mGal for gravity anomalies at
	a spatial resolution of 100 km.},
  doi = {10.1002/2014GL061904},
  keywords = {GOCE, Earth's gravity field determination, spherical harmonic model}
}