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History of modifications
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List of datasets covered by this document
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Acronyms
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General definitions
Equivalent Water Height: Equivalent Water Height represents the mass change per unit area as if it were entirely due to a uniform layer of water. It is derived from changes in gravity and surface deformation and is typically expressed in millimetres or centimetres.
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Water Storage Compartment (WSC): A WSC refers to a distinct component of the terrestrial water cycle in which water is stored, such as groundwater, soil moisture, surface water, snow, or glaciers. In the context of GWSC, the individual WSCs, i.e. glacier mass change (GM), snow water equivalent (SWE), root zone soil moisture (RZSM), and surface water storage (SWS), are subtracted from the TWSA signal to isolate the groundwater storage change signal.
Executive summary
This Product User Guide and Specifications (PUGS) is a self-contained document that gathers all necessary information for using and applying the Groundwater Storage Change (GWSC) dataset, as delivered within the Copernicus Climate Change Service (C3S).
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This document provides a brief summary of the data processing involved in generating the GWSC dataset in Section 1.1. A more extensive description of the data processing algorithm can be found in the GWSC Algorithm Theoretical Basis Document (ATBD). This section also includes details on the spatial and temporal characteristics of the product. Section 1.2 then details the Global Climate Observing System (GCOS) user requirements and their fulfilment with the dataset. This is followed by an example visualisation of key variables in Section 1.3. Section 1.4 collects data usage information, including the known issues and limitations of the GWSC dataset in Section 1.4.4, which are especially relevant for users unfamiliar with gravity-based groundwater products. This document concludes with Section 2, which provides information on data access.
Product Description
Groundwater Storage Change (GWSC) description
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Groundwater storage change (GWSC) refers to variations in the amount of water stored in aquifers and subsurface reservoirs. Groundwater is the largest liquid freshwater reservoir on Earth and plays a central role in sustaining ecosystems, agriculture, and fresh water supply, and, as such, has been designated as an Essential Climate Variable (ECV) by the World Meteorological Organization (WMO). GWSC is a key indicator of long-term changes in water availability, particularly in regions where surface water resources are limited or seasonally variable.
Figure 1 provides a schematic illustration of the global hydrological cycle, highlighting the water storage compartments making up Terrestrial Water Storage (TWS) and the role of groundwater in it.
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The groundwater signal is derived by subtracting observation- and model-based estimates of the anomalies A of other Water Storage Compartments (WSCs), i.e. glacier mass (GM), snow water equivalent (SWE), root zone soil moisture (RZSM), and surface water storage (SWS), from the TWSA, following the water budget equation (1):
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It should be noted that Greenland and Antarctica are excluded from the GWSC product. In these regions, the TWSA signal is dominated by changes in glacier and ice sheet mass, which are very large in magnitude and carry substantial uncertainties. As a result, reliably isolating the groundwater signal through the subtraction approach is not currently feasible for these regions.
Data processing algorithm
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The GWSC product is derived from five input data streams: the C3S TWSA and the four WSC datasets covering glacier mass change (GM), snow water equivalent (SWE), root zone soil moisture (RZSM), and surface water storage (SWS). Figure 2 provides an overview of the processing steps required to produce the GWSC data. Comprehensive details of the algorithm are available in the GWSC ATBD. The current version of the algorithm is GWSC v1.0.
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Figure 2: Overview of the processing steps in the GWSC production system. Input WSC data streams (TWSA, SWS, SWE, RZSM, GM) and their uncertainties are converted to anomalies, resampled to a common 0.5° grid under a consistent land-ocean mask, filtered with a 250 km Gaussian filter, whose width is informed by a spatial correlation analysis, and finally combined through the subtraction approach. Uncertainties are propagated throughout the chain to the final GWSC product.
Product characteristics
Processing level
The processing level of the GWSC product is Level-4 according to the definition by NASA EarthDATA1 .
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1 (https://www.earthdata.nasa.gov/learn/earth-observation-data-basics/data-processing-levels, visited 29.04.2026) |
Spatial information
The Level-4 data are provided on a regular 0.5° x 0.5° latitude-longitude grid. This results in a dimension of 720 grid cells in longitude and 360 in latitude for the data fields. Of these 259200 grid cells in total, 59018 are considered land cells according to the applied land-ocean mask and contain numeric values, whereas the remaining cells contain NaN (Not a Number) values. The mask is based on the European Space Agency (ESA) Climate Change Initiative (CCI) global map of open water bodies v4.0 (CCI WB v4.0) and are freely available in different resolutions (Sharifi et al., 2025b).
Longitude and latitude values are expressed with respect to the WGS84 ellipsoid. The given coordinates describe the central point of each grid cell.
Temporal information Anchor sec_temporal sec_temporal
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Typically, the GWSC product has a monthly temporal resolution. The time variable of the product is based on the time variable of the TWSA product. In TWSA it represents the mean day of the data collection period used for each monthly value. Therefore, the time stamp in the TWSA product corresponds to the 15th or 16th of the respective month. In the GWSC product the timestamp is set to the 1st of the respective month for user friendliness.
It has to be noted that, due to GRACE and GRACE-FO mission operations or instrument issues, some months are unavailable, or of lower data quality, or based on data collection periods that deviate from full monthly coverage. Additionally, owing to the gap between the two missions GRACE and GRACE-FO no data are available between July 2017 and May 2018. Since the GWSC product is based on the GRACE-based TWSA product, the corresponding months are also missing in the GWSC product. Figure 3 shows all available monthly solutions. For more details on the deviations from the monthly solutions, including missing data, monthly solutions with poorer data quality, and solutions where the data collection deviated from the monthly time frame, please refer to section 1.1.2.3 of the TWSA PUGS.
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Figure 3: Overview of the available monthly GWSC fields for Climate Data Record (CDR) v1.0.
Timeliness and update frequency
The GWSC data processing chain is mainly dominated by a) the production schedule of the TWSA dataset, and b) the delivery of the Glacier Mass product. The former requires approximately three months from data collection of the satellites to the generation of Level-3 TWSA data. For the latter case, however, a full global product can only be produced once a year. This is due to the fact that manual measurements of the changes of glacier heights, which are crucial to the production, are usually only done once a year, around the same dates. As soon as both these datasets are available, the GWSC processing chain takes only a couple of days to run on GFZ's HPC cluster. Accordingly, the last entry of the dataset dates back to the latest month that both datasets cover.
CDR v1.0 covers the period from April 2002 to September 2023. CDR v2.0 will be published in early 2027 and extend this period until September 2026. An ICDR will be published in early 2028 and, again, extend the period until September 2027.
Overview of Product Target Requirements Anchor gwsc_gcos gwsc_gcos
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The product target requirements have been defined by the GCOS (WMO, 2025). Table 1 summarises the requirements and characteristics of the C3S GWSC product.
For each requirement, a threshold and a goal value, for some also a breakthrough value, are defined as listed in Table 1. The goal is the ideal level. Once this is met, further improvements in that criterion are not strictly necessary for most applications. Breakthrough is the level considered a major step towards operational provision. Threshold is the minimum acceptable requirement. Further details on product accuracy and stability are provided in the Product Quality Assessment Report (PQAR).
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Example visualisation of key variables Anchor gwsc_results gwsc_results
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Figure 4 shows, as an example, (a) GWSC and (b) GWSC uncertainty for March 2008.
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Figure 4: Fields of the final data product. (a) shows GWSC from the final data product for the example month of March 2008 stored in the gwsc variable in the netcdf file; (b) shows the uncertainty of GWSC for the same month, stored in the gwsc_uncertainty variable of the netcdf file.
Data usage information
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Data format and file naming
The data file is in "NetCDF-4" format and is CF-Convention v1.8 compliant. The data are delivered as a zip archive containing the NetCDF file.
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The data set file name for both CDRs and ICDRs follows the following naming convention, with the tokens of the filename provided in Table 2:
GGG_HHH_III_KKK_LLLMMM_NNNOOO_PPP.nc
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Contains the global grid of monthly GWSC data, version 1.0. The temporal coverage spans from April 2002 to September 2023.
Quality flags and data masks
The dataset does not come with quality flags. However, some of the input datastreams do provide such information. TWSA provides a flag for the filter used in individual months, described in section 1.4.2 of the TWSA PUGS. SWE provides a flag describing reasons for missing data, like over mountains or open water, described in section 1.4.2 of the SWE PUGS. RZSM comes with a variety of quality flags. See section 1.7 of the RZSM PUGS for a summary. GM and SWS do not provide such information.
For information on masking see section 1.1.1 of this document and sections 2.6.1 and 3. of the GWSC ATBD.
File contents
The data is provided as a single netCDF file of the size of 187.8 MB for the entire time series.
File dimensions
The file dimensions are detailed in Table 3 below.
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File variables
The variables in the netCDF file are summarised in Table 4, and more details are provided below.
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File metadata
The netCDF file contains descriptive metadata as global attributes (Table 5 for all attributes and their values).
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Examples of known climate applications and best practices
As a new C3S dataset, the C3S GWSC product has not yet been used in climate applications. However, the preceding dataset of the Global Gravity-based Groundwater Project (G3P) has been used in validation studies, such as Sayyadi et al. (2025) or Güntner et al. (2026), and in climate-related studies, such as Ongdas et al. (2025).
Additionally, the value of the G3P dataset has been demonstrated on https://www.globalwaterstorage.info/en/ (last accessed April 21, 2026), an information portal dedicated to the GRACE and GRACE-FO satellite missions, their applications and derived products. Application examples are showcased through blog articles written by scientists from the community, as well as a regularly featured “picture of the month".
Known Issues and Limitations
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Some principal limitations of GWSC stem from the input TWSA product and the nature of GRACE-based observations. Those are the limited spatial resolution of approximately 250–300 km, the coarse temporal resolution of one month, the missing months, and the phenomenon known as leakage. For more details on this please refer to section 1.4.5 of the TWSA PUGS.
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Greenland and Antarctica are excluded from the GWSC product. In these regions, the input TWSA signal is dominated by changes in glacier and ice sheet mass, which are very large in magnitude and carry substantial uncertainties. As a result, reliably isolating the groundwater signal through the subtraction approach is currently not feasible for these regions.
Data access information
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GWSC data
The GWSC data is available through the Copernicus Climate Data Store (CDS) web-based service (https://cds.climate.copernicus.eu/). To access the CDS and all its toolbox software, a free-of-charge registration is required. Data can be directly downloaded from the portal and used under the License to Use Copernicus Products (also included on the download page). All requests for user support shall be directed via the ECMWF Support Portal.
Input and auxiliary data
The TWSA input data is available from the TWSA CDS page (URL last accessed on 21.04.2026).
For all other input and auxiliary datasets please refer to the GWSC ATBD.
Data citation requirements
Same as landing page once this is agreed with ECMWF/CDS
User Support
A dedicated support portal (https://confluence.ecmwf.int/site/support) has been set up by the Copernicus User Support (CUS) team, which provides support to users of the Copernicus Atmosphere Monitoring Service (CAMS) and C3S services at ECMWF. All enquiries about the GWSC dataset can be submitted through the service desk where appropriate agents will deal with it. Once submitted, the user may add comments or further information to the issue, including responding to questions / requests for additional information from the support team.
References
- Güntner, A., Sharifi, E., Haas, J., Boergens, E., Cao, F., Dahle, C., Darbeheshti, N., Dobslaw, H., Dussaillant, I., Dorigo, W., Flechtner, F., Jäggi, A., Kosmale, M., Lasser, M., Luojus, K., Meyer, U., Pasik, A., Preimersberger, W., Ruz Vargas, C., and Zemp, M., 2026. The Global Gravity-based Groundwater Product (G3P), Earth Syst. Sci. Data Discuss. [preprint], https://doi.org/10.5194/essd-2025-797 (URL last accessed 29/04/2026), in review.
- Ongdas, N., Yapiyev, V., Catalin, S., Mehan, S., Muzdybaev, M., Hartmann, A., 2025. Lowland transboundary river in a cold, semi-arid steppe: review of the Yesil River basin. nviron Earth Sci 84, 496. https://doi.org/10.1007/s12665-025-12500-0 (URL last accessed 29/04/2026)
- Sayyadi, S., Nguyen, V., Apel, H., Haas, J., Dang, T. T., Than, V. D., Nguyen, N. H., Güntner, A., 2025. Observation-based analysis of groundwater storage in Vietnam’s Central Highlands: influence of hydro-climatic variability. Hydrological Sciences Journal, 70, 16, 2993-3012. https://doi.org/10.1080/02626667.2025.2568558 (URL last accessed 29/04/2026)
- Sharifi, E., Haas, J., Boergens, E., Dobslaw, H., and Güntner, A., 2025a. Technical note: GRACE-compatible filtering of water storage data sets via spatial autocorrelation analysis, Hydrol. Earth Syst. Sci., 29, 6985–6998, https://doi.org/10.5194/hess-29-6985-2025 (URL last accessed 29/04/2026)
- Sharifi, Ehsan; Haas, Julian; Boergens, Eva; Güntner, Andreas, 2025b. Global Multi-Resolution Land Fraction and Land–Ocean Masks Derived from ESA CCI Water Bodies v4.0 (Version 1.0). GFZ Data Services. https://doi.org/10.5880/G3P.2023.001 (URL last accessed 29/04/2026)
- WMO, 2025. The 2022 GCOS ECVs Requirements, 2022 edition - Updated in 2025, https://library.wmo.int/idurl/4/58111 (URL last accessed 29/04/2026)
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This document has been produced in the context of the Copernicus Climate Change Service (C3S). The activities leading to these results have been contracted by the European Centre for Medium-Range Weather Forecasts, operator of C3S on behalf of the European Union (Delegation Agreement signed on 11/11/2014 and Contribution Agreement signed on 22/07/2021). All information in this document is provided "as is" and no guarantee or warranty is given that the information is fit for any particular purpose. The users thereof use the information at their sole risk and liability. For the avoidance of all doubt , the European Commission and the European Centre for Medium - Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view. |
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