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Observing Earth’s magnetic environment with the GRACE-FO mission [PDF]

open access: yesEarth, Planets and Space, 2021
The Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission carries magnetometers that are dedicated to enhance the satellite’s navigation.
C. Stolle   +7 more
doaj   +7 more sources

Acceleration of Dynamic Ice Loss in Antarctica From Satellite Gravimetry [PDF]

open access: yesFrontiers in Earth Science, 2021
The dynamic stability of the Antarctic Ice Sheet is one of the largest uncertainties in projections of future global sea-level rise. Essential for improving projections of the ice sheet evolution is the understanding of the ongoing trends and ...
Theresa Diener   +7 more
doaj   +3 more sources

A GRACE-FO első másfél éve [PDF]

open access: yesGeodézia és Kartográfia, 2020
A GRACE-műholdak 2002 és 2017 között hónapos felbontásban szolgáltatták a Föld nehézségi erőterének időbeli változásait, lehetőséget nyújtva ezzel a nagyobb tömegátrendező folyamatok hatásának műholdas követésére.
Lóránt Földváry, Annamária Nyilas
openaire   +4 more sources

GRACE-FO processing at IfE/LUH [PDF]

open access: yes, 2021
Processing strategy of the LUH-GRACE-FO-2020 monthly gravity field time series is presented. The spectral noise, spatial noise and signal content of the time series (2018-06 - 2020-08) is evaluated.
Koch, Igor   +3 more
openaire   +4 more sources

Filling the GRACE/-FO gap of mass balance observation in central west Greenland by data-driven modelling

open access: yesAnnals of Glaciology
Continuous monitoring of the mass balance of the Greenland ice sheet is crucial to assess its contribution to the rise of sea levels. The GRACE and GRACE-FO missions have provided monthly estimates of the Earth’s gravity field since 2002, which have been
Anna Puggaard   +4 more
doaj   +2 more sources

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

open access: yesEarth System Science Data, 2017
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.
N. Darbeheshti   +5 more
doaj   +4 more sources

GRACE-FO Satellite Data Preprocessing Based on Residual Iterative Correction and Its Application to Gravity Field Inversion. [PDF]

open access: yesSensors (Basel)
To address the limited inversion accuracy caused by low-fidelity data in satellite gravimetry, this study proposes a data preprocessing framework based on iterative residual correction.
Zhao S, Li L.
europepmc   +2 more sources

The analysis on groundwater storage variations from GRACE/GRACE-FO in recent 20 years driven by influencing factors and prediction in Shandong Province, China. [PDF]

open access: yesSci Rep
Monitoring and predicting the regional groundwater storage (GWS) fluctuation is an essential support for effectively managing water resources. Therefore, taking Shandong Province as an example, the data from Gravity Recovery and Climate Experiment (GRACE)
Li W   +11 more
europepmc   +2 more sources

Advancements in the GRACE and GRACE‐FO Gradiometer Mode

open access: yesEarth and Space Science
AbstractThe global gravitational gradient field has not been observed since the decommission of GOCE in 2013. Based on the foundational work of Peidou and Pagiatakis (2019, https://doi.org/10.1029/2018jb016382), we advance the concept of GRACE gradiometer mode (GM) for the purpose of using GRACE, GRACE‐FO and future gravity space missions as ...
Nikeet Pandit, Spiros D. Pagiatakis
openaire   +2 more sources

Frequency-Dependent Scaling Factors to Estimate Multiple Time-Period Global Mass Changes Observed by GRACE/GRACE-FO

open access: yesIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
The scaling factor method is commonly used to restore near-true time-variable gravity from gravity recovery and climate experiment/follow-on (GRACE/GRACE-FO).
Zhenran Peng   +3 more
doaj   +2 more sources

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