GLEAM4: global land evaporation and soil moisture dataset at 0.1 resolution from 1980 to near present. [PDF]
Miralles DG +10 more
europepmc +1 more source
High-resolution temporal gravity field data products: Monthly mass grids and spherical harmonics from 1994 to 2021. [PDF]
Uz M +5 more
europepmc +1 more source
Evaluating GNSS infrastructure readiness for IGS contribution: the case of King Sejong Station, Antarctica. [PDF]
Lee SJ, Yun HS, Yoon HM, Lee SH.
europepmc +1 more source
Spatial-domain combination of GRACE monthly time-variable gravity models based on multiple weighting strategies and comparison of models' performance in the Caspian Sea. [PDF]
You W +7 more
europepmc +1 more source
Substantial increase of organic carbon storage in Chinese lakes. [PDF]
Liu D +10 more
europepmc +1 more source
GLEAM4: global land evaporation dataset at 0.1° resolution from 1980 to near present
Miralles DG +10 more
europepmc +1 more source
Related searches:
Future Satellite Gravimetry for Geodesy
Earth, Moon, and Planets, 2004After GRACE and GOCE there will still be need and room for improvement of the knowledge (1) of the static gravity field at spatial scales between 40 km and 100 km, and (2) of the time varying gravity field at scales smaller than 500 km. This is shown based on the analysis of spectral signal power of various gravity field components and on the ...
Flury, J., Rummel, R.
openaire +3 more sources
GOCE, Satellite Gravimetry and Antarctic Mass Transports
Surveys in Geophysics, 2011In 2009 the European Space Agency satellite mission GOCE (Gravity Field and Steady-State Ocean Circulation Explorer) was launched. Its objectives are the precise and detailed determination of the Earth’s gravity field and geoid. Its core instrument, a three axis gravitational gradiometer, measures the gravity gradient components V
R. Rummel +5 more
openaire +3 more sources
Rosborough Representation in Satellite Gravimetry
2015Rosborough representations are known from and used in satellite altimetry. The radial orbit perturbation is represented in spherical coordinates and separated into a geographically mean (ascending plus descending) and a geographically variable (ascending minus descending) part. This principle is easily generalized to any functional of the gravitational
Nico Sneeuw, Mohammad A. Sharifi
openaire +1 more source

