Please Note: This dataset is retired, and is displayed for archive purposes only, and may not reflect the most updated information.
JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height Release 06 Version 02
(TELLUS_GRAC-GRFO_MASCON_GRID_RL06_V2)
7 Publications Cited this Dataset
Citation metrics available for years (2014-2021)
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Publications citing JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height Release 06 Version 02
Citation metrics available for years (2014-2021)
Year | Citation |
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2020 | Wiese, D. N., Yuan, D.-N., Boening, C., Landerer, F. W., and Watkins, M. M.: JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height JPL Release 06 Version 02, available at: https://podaac.jpl.nasa.gov/dataset/TELLUS_GRAC-GRFO_MASCON_GRID_RL06_V2?ids= Collections:ProcessingLevel:Platform&values=GRACE-FO: *3*:GRACE&search=%22GRACE-FO%22, last access: February 2017. Global partitioning of runoff generation mechanisms using remote sensing data, Hydrology and Earth System Sciences,https://doi.org/10.5194/hess-24-1415-2020 |
2020 | Wiese, D. N., Yuan, D.-N., Boening, C., Landerer, F. W. and Watkins, M. M. JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height JPL Release 06 Version 02. Ver. 2. PO. DAAC, CA, USA, 2019. Relative importance of increased atmospheric CO2 concentration and local moisture deficit to hot extremes, Hydrology and Earth System Sciences,https://doi.org/10.5194/hess-2020-400 |
2021 | Analysis of the interannual variability in satellite gravity solutions: detection of climate modes in water mass displacements across continents and oceans, Journal,10.1007/s00382-021-05953-z |
2021 | Mechanical response of shallow crust to groundwater storage variations: Inferences from deformation and seismic observations in the Eastern Southern Alps, Italy, Journal,10.1029/2020JB020586 |
2021 | Wiese, D., Yuan, D., Boening, C., Landerer, F., and Watkins, M. (2019). JPL GRACE and GRACE-FO mascon ocean, ice, and hydrology equivalent water height RL06M CRI filtered version 2.0 filtered version 2.0. Dataset accessed [2020-12-30] at https://doi.org/10.5067/temsc-3mj62, JPL Physical Oceanography Distributed Active Archive Center. Modeling the Interconnectivity of Non-stationary Polar Ice Sheets, Preprint,10.2139/ssrn.3912725 |
2021 | Wiese, D.N., Yuan, D.N., Boening, C., Landerer, F.W., Watkins, M.M., 2018. JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height JPL Release 06 Version 02. Ver. 2. PO.DAAC, CA, USA, https://doi.org/10.5067/TE MSC-3MJ62. Dataset accessed [2021-01-15] Sub-regional groundwater storage recovery in North China Plain after the South-to-North water diversion project, Journal,10.1016/j.jhydrol.2021.126156 |
2021 | The Anthropocene by the Numbers: A Quantitative Snapshot of Humanity's Influence on the Planet, Preprint,10.48550/arXiv.2101.09620 |
DOI | 10.5067/TEMSC-3MJ62 |
Short Name | TELLUS_GRAC-GRFO_MASCON_GRID_RL06_V2 |
Description | This dataset contains gridded monthly global water storage/height anomalies relative to a time-mean, derived from GRACE and GRACE-FO and processed at JPL using the Mascon approach (Version2/RL06). These data are provided in a single data file in netCDF format, and can be used for analysis for ocean, ice, and hydrology phenomena. The water storage/height anomalies are given in equivalent water thickness units (cm). The solution provided here is derived from solving for monthly gravity field variations in terms of geolocated spherical cap mass concentration functions, rather than global spherical harmonic coefficients. Additionally, realistic geophysical information is introduced during the solution inversion to intrinsically remove correlated error. Thus, these Mascon grids do not need to be destriped or smoothed, like traditional spherical harmonic gravity solutions. The complete Mascon solution consists of 4,551 relatively independent estimates of surface mass change that have been derived using an equal-area 3-degree grid of individual mascons. It should be noted that this dataset does not correct for leakage errors across coastlines; it is therefore recommended only for users who want to apply their own algorithm to separate between land and ocean mass very near coastlines. Please refer to the 'Data Access' tab at the top of this page to gain direct access to the Mascon data. For more information, please visit https://grace.jpl.nasa.gov/data/get-data/jpl_global_mascons/. For a detailed description on the Mascon solution, including the mathematical derivation, implementation of geophysical constraints, and solution validation, please see Watkins et al., 2015, doi: 10.1002/2014JB011547. This product is intended for expert use only; other users are encouraged to use the CRI-filtered Mascon dataset, which is available here: https://podaac.jpl.nasa.gov/dataset/TELLUS_GRACE_MASCON_CRI_GRID_RL06_V2. |
Version | RL06Mv02 |
Dataset Type | DEPRECATED |
Questions related to this dataset? Contact podaac@podaac.jpl.nasa.gov
Please contact podaac@podaac.jpl.nasa.gov for more info.
Citation is critically important for dataset documentation and discovery. Please cite the data as follows, and cite the reference papers when it is appropriate.
Citation | D. N. Wiese, D.-N. Yuan, C. Boening, F. W. Landerer, M. M. Watkins. 2019. JPL GRACE and GRACE-FO Mascon Ocean, Ice, and Hydrology Equivalent Water Height. Ver. RL06Mv02. PO.DAAC, CA, USA. Dataset accessed [YYYY-MM-DD] at https://doi.org/10.5067/TEMSC-3MJ62
For more information see Data Citations and Acknowledgments.
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Journal Reference | Watkins, M. M., D. N. Wiese, D.-N. Yuan, C. Boening, F. W. Landerer. 2015. Improved methods for observing Earth's time variable mass distribution with GRACE, JGR Solid Earth, 120, 4. 10.1002/2014JB011547 |