The gravity field model ITSG-Grace2016 ====================================== T. Mayer-Guerr, B. Klinger, A. Kvas, N. Zehentner, M. Ellmer http://ifg.tugraz.at/downloads/gravity-field-models/itsg-grace2016 Unconstrained monthly solutions ------------------------------- For each month of the observation period sets of spherical harmonic coefficients for different maximum degrees (60, 90, 120) were estimated without applying any regularization. Daily variations are co-estimated and eliminated from the normal equations. For most applications a spectral resolution of degree 60 is sufficent. In some cases a higher resolution is preferrable but in some rare months the orbit configuration dont allow to solve for high degrees. Processing Details ------------------ The ITSG-Grace2016 gravity field solutions are computed using variational equations with an arc length of 24 hours. In addition to satellite state, instrument calibration and static/long-term spherical-harmonic coefficients, daily gravity field variations up to degree and order 40 were modelled in the adjustment process. K-band range rates with a sampling of 5 seconds and kinematic orbits with a sampling of 5 minutes were used as observations. The kinematic orbits of the GRACE satellites (Zehentner and Mayer-Gürr 2015) were processed using the GPS orbits and clock solutions provided by IGS. An improved attitude product derived from a combination of star camera data and angular accelerations (Klinger and Mayer-Gürr 2014) was used. Additionally, accelerometer scale factor were estimated per axis and day. The accelerometer bias were modelled as cubic splines of degree 3 per axis with nodal points every 6 hours. The following background models were used during the data processing: Earth rotation: IERS 2010 Moon, sun and planets ephem.: JPL DE421 Earth tide: IERS 2010 Ocean tide: EOT11a Pole tide: IERS 2010 Ocean pole tide: Deasi 2003 (IERS 2010) Atmospheric tides (S1, S2): van Dam and Ray 2010 Atmosphere and Ocean Dealiasing: AOD1B RL05 Relativistic corrections: IERS 2010 Permanent tidal deformation: included (zero tide) The above models were reduced during the analysis process. They are not present in the solutions. The models are provided as mean value over the specific time spans (daily, monthly) in the background directory.