-
(Figure 3) Rate of mass change for July for years 2004, 2010, 2012 and 2019 f...
This dataset has no description
-
(Figure 2) Biennial mass balance and its components from GRACE/GRACE-FO and S...
Biennial mass balance anomaly wrt 2003-2018 mean. -
(Figure 1) Monthly mass changes of the Greenland Ice Sheet from SMB-D (origin...
Relative changes in respect to mean value. -
(Figure 1) Monthly mass changes of the Greenland Ice Sheet from GRACE/GRACE-FO
Relative changes in respect to mean value. -
GRACE monthly solutions for evaluation of background
These time series are supplementary material to the paper Kvas and Mayer-Gürr: GRACE gravity field recovery with background model uncertainties. -
AIUB-G3P GRACE monthly gravity field solutions
GRACE monthly gravity field solutions starting from April 2002 to June 2017 up to degree and order 90 computed with the Celestial Mechanics Approach at AIUB. The time series... -
ITSG-Grace2016 - Monthly and Daily Gravity Field Solutions from GRACE
The ITSG-Grace2016 gravity field model is the latest GRACE only gravity field model computed at Graz University of Technology, providing unconstrained monthly and Kalman... -
IGG-SLR-HYBRID: High-resolution temporal gravity fields from satellite laser ...
Monthly gravity fields from satellite laser ranging using a hybrid parametrization including spherical harmonic coefficients and empirical orthogonal functions from GRACE -
ITSG-Grace2018 - Monthly, Daily and Static Gravity Field Solutions from GRACE
The ITSG-Grace2018 gravity field model is the latest GRACE-only gravity field model computed at Graz University of Technology, providing unconstrained monthly and regularized... -
EIGEN-6S4 A time-variable satellite-only gravity field model to d/o 300 based...
EIGEN-6S4 (Version 2) is a satellite-only global gravity field model from the combination of LAGEOS, GRACE and GOCE data. All spherical harmonic coefficients up to degree/order... -
The Combined Gravity Model GGM05C
GGM05C is an unconstrained global gravity model complete to degree and order 360 determined from 1) GRACE K-band intersatellite range-rate data, GPS tracking and GRACE... -
ITU_GGC16 The combined global gravity field model including GRACE & GOCE data...
ITU_GGC16 is a static global gravity field model up to degree order 280 computed from the combination of ITU_GRACE16 (up to d/o 180) and GO_CONS_GCF_2_TIM_R5 (up to d/o 280) by... -
ITU_GRACE16 The global gravity field model including GRACE data up to degree ...
ITU_GRACE16 is a static global gravity field model up to degree order 180 computed from GRACE SST data of 50 months collected between April 2009 to October 2013 by collaboration... -
WHU-SWPU-GOGR2022S: A combined gravity model of GOCE and GRACE
WHU-SWPU-GOGR2022S is a static gravity field model complete to spherical harmonic degree and order of 300 by combining GOCE and GRACE normal equations. Details of the processing... -
HUST-Grace2020: Monthly gravity field model derived from GRACE mission
The HUST-Grace2020 model is the latest GRACE-only gravity field solution developed at Huazhong University of Science and Technology. The model includes a set of spherical... -
WHU-GRACE-GPD01s: Monthly gravity field models derived from GRACE intersatell...
The WHU-GRACE-GPD01s models are the latest monthly gravity field solutions recovered from GRACE intersatellite geopotential difference (GPD) data processed at the School of... -
SWPU-GRACE2021: a new temporal gravity model from GRAC
The new unconstrained GRACE monthly solution SWPU-GRACE2021 is recently developed with the dynamic approach. The reprocessed GRACE L1B RL03 data and de-aliasing product AOD1B... -
The satellite-only gravity field model GOCO06s
GOCO06s is a satellite-only, global gravity field model up to degree and order 300, with secular and annual variations up to degree and order 120. It was produced by the GOCO... -
ESA’s Release 6 GOCE gravity field model by means of the direct approach base...
"ESA’s Release 6 GOCE gravity field model by means of the direct approach based on improved filtering of the reprocessed gradients of the entire mission (GO_CONS_GCF_2_DIR_R6)"... -
Using real polar terrestrial gravimetry data to overcome the polar gap proble...
With the successful completion of ESA's PolarGAP campaign, terrestrial gravimetry data (gravity anomalies) are now available for both polar regions. Therefore, it is now...