CSR Release-06.1-LRI GRACE-FO Level-2 Data Products
Thank you for your interest in the latest, Release-06.1-LRI GRACE-FO Level-2 data products.
This page describes the RL06.1 time-series of monthly time-variable gravity field estimates obtain using the satellite-2-satellite ranging observation from the Laser Ranging Interferometer instrument. The description on this page is presently intended for users already familiar with the nomenclature and use of GRACE and GRACE-FO Level-2 data products.
The CSR RL06.1-LRI Level-2 data products are available for June 2018 onwards. Due to interruption in the data collection, the RL06.1-LRI products do not exist for the following months: August 2018 through November 2018, February 2019, March 2019, July 2022 and August 2022. The RL06.1-LRI data products include the GSM, GAC and GAD data products. The GAC and the GAD products may vary from the ones delivered as part of the RL06.1 products (KBR) because the days included in either set of product may differ.
The CSR RL06.1-LRI Level-2 data products can be downloaded here.
Information Content in RL06.1-LRI GSM Files:
The information content in RL06.1-LRI GSM files is the same as in the RL06 (and RL06.1) GSM files from KBR. That is, the RL06.1-LRI GSM files represent the total gravity variability due to land surface hydrology, cryospheric changes, episodic (earthquake) processes, glacial isostatic adjustment (GIA), and corrections to the background models for atmospheric and oceanic processes. The RL06.1-LRI GSM products can be used in the same way as RL06 and RL06.1 GSM products.
Level-2 Data Products:
For each calendar month, in general four product files are available. For example, for the month of June 2018, the available products are:
The product files GSM-2* contains the coefficients for the Earth gravity field for the indicated span. The monthly gravity field solutions are unconstrained where the unconstrained gravity parameters are estimated seperately from other orbit related parameters. ONLY the formal error standard deviations (sigmas) of the estimated geopotential harmonics are contained in the GSM-2* products. The use of a suitable truncation or smoothing technique is recommended. Examples are available in the literature. The selection of the smoothing technique and the highest degree are left to the user's discretion. Users desirous of replacing the C20 and C30 values of the GSM file with improved estimates are offered the option of using SLR-determined C20 and C30 values given in GRACE Technical Note - 14.
The product file GAC-2 contains the average of the Release-06 AOD1B product for the ensemble of days as used in creating the monthly solution. Although this file contains the degree 0 and degree 1 harmonics for completeness, these harmonics were NOT used in Level-2 data processing. The averaging is carried using the whole days - regardless of whether full or partial day's data were used in creating the monthly solution.
The product file GAD-2 represents the mean ocean bottom pressure. Please review the AOD1B Product Description Document for its complete definition and usage guidelines. Over the oceans, maps of GAC and GAD products will look the same only if degree 0 and degree 1 terms are included while drawing both the maps. Note, however, that degree-0 and degree-1 of the AOD products (from which GAC is derived) were not used in Level-2 data processing. The GAD* products were not used in GRACE data processing, and are provided only as a service to the user community.
The fields definition of the Level-2 filenames have comply with GRACE-FO filename conventions. Please refer to the Level-2 handbook and RL06.1 Release Notes for more details.
A GRACE-FO Level-2 gravity field product is a set of spherical harmonic coefficients of the exterior geopotential. A product name is specified as
PID is 3-character product identification mnemonic
-2 denotes a GRACE Level-2 product
YYYYDOY-YYYYDOY specifies the date range (in year and day-of-year format) of the data used in creating this product
dddd specifies the gravity mission
sssss is an institution specific string
mmmm is a 4-character mnemonic used to identify the characteristics of the gravity solution
rrvv is a 2-digit (leading-zero-padded) release number and 2-digit (leading zero-padded) version number
The Product Identifier mnemonic (PID) is made up of one of the following values for each of its 3 characters:
= G: Geopotential coefficients
= S: Estimate made from only GRACE-FO data
= A: Average of any background model over a time period
= M: Estimate of the Static field.
= C: combination of non-tidal atmosphere and ocean (for details of combination see AOD1B Description Doc)
= D: bottom-pressure over oceans, zero over land (for details of combination, see AOD1B Description Doc)
The ‘dddd’ string specifies the gravity mission:
= GRFO: Gravity Recovery and Climate Experiment Follow-On
The ‘sssss’ string specifies the institute where the data were processed:
= UTCSR: The University of Texas at Austin Center for Space Research
The ‘mmmm’ string is a 4-character mnemonic used to characterize the gravity solution. The first character is used to identify the primary observation type used in the gravity solution (Note: MWI = Microwave Instrument). The second character defines the size of the spherical harmonic expansion in the file. The third and fourth characters are used to represent other characteristics of the gravity solution, including the type of basis function used, whether it is an unconstrained or constrained solution, and the type of windowing function used. For any files that describe the average of a background model (where ‘A’ is the 2nd character in the PID), only the 2nd character in the ‘mmmm’ string is defined/applicable. The 1st, 3rd, and 4th characters are set to be equivalent to the corresponding gravity solution.
= A: 60 x 60 spherical harmonic expansion
= B: 96 x 96 spherical harmonic expansion
3rd and 4th Characters
= 01: unconstrained spherical harmonic solution with a boxcar windowing function
The ‘rrvv’ string indicates the release (rr) and version (vv) of the solution. The release number is tied to a specific set of background force models, and indicates consistency between solutions across different missions. The version number indicates the version of the solution under a specific release.
Consistent with GRACE, GRACE-FO is not sensitive to degree 1 harmonics (geocenter). GRACE/GRACE-FO Technical Note TN-13 contains geocenter estimates using the methods of Swenson et al.  and Sun et al. , and is updated in synch with Level-2 monthly releases. These have been reprocessed for the entire GRACE and GRACE-FO time span to be consistent with the below-mentioned TN-14, so users need to replace the entire TN-13 time series. It is recommended to augment the GRACE and GRACE-FO geocenter with this product for surface mass change estimation.
Consistent with the GRACE SDS recommendations, GRACE-FO SDS recommends the replacement of the native GRACE-FO C20 coefficient with that from SLR using the GRACE/GRACE-FO Technical Note TN-14. GRACE/GRACE-FO Technical Note TN-14 contains both C20 and C30 estimates derived from SLR and using Level-2 RL06 standards and is updated in synch with Level-2 monthly releases. It is recommended to replace/substitute the native GRACE and GRACE-FO C20 coefficients with this product [Loomis et al., 2019] for all months.
The GRACE-FO SDS has determined that the C30 coefficient in GRACE-FO shows comparatively more variability relative to the long-term climatology derived from the GRACE C30 coefficient. Therefore, SDS recommends that users assess the impact on regional mass budgets of substituting the GRACE-FO C30 coefficient with one derived from SLR (similar to the C20 approach). GRACE/GRACE-FO Technical Note TN-14 is now provided and contains both C20 and C30 estimates derived from SLR and using Level-2 RL06 standards, updated in synch with Level-2 monthly releases. It is recommended to replace/substitute the native GRACE and GRACE-FO C30 coefficients with this product [Loomis et al., 2020] from 08/2016 onwards.
When using the CSR RL06.1-LRI products, please acknowledge that the data was downloaded from doi:10.5067/GFL20-LC061 and cite:
Pie, N., Bettadpur, S. V., Tamisiea, M., Krichman, B., Save, H., Poole, S., et al. (2021). “ Time variable Earth gravity field models from the first spaceborne laser ranging interferometer”. Journal of Geophysical Research: Solid Earth, 126, e2021JB022392. https://doi.org/10.1029/2021JB022392.
ACCESS THE RL06.1-LRI PRODUCTS.
Feedback is Requested:
The GRACE-FO project SDS is looking for feedback from the Science Team and wider community on the these new RL06.1 gravity fields derived from the LRI ranging observation. Note that due to interruption in the LRI data collection a few monthly RL06.1-LRI solutions are expected to perform poorer than their KBR couterparts. For more details, see Pie, et al (JGR, 2021) and Pie, et al (AGU Fall 2022).
Further Details on CSR Level-2 Processing Standards
Please revisit these pages for further information.