Index of /L2B_UNC

[ICO]NameLast modifiedSizeDescription

[PARENTDIR]Parent Directory  -  
[DIR]v1.0/2026-01-07 18:16 -  
[DIR]v2.0/2026-02-18 15:47 -  
[DIR]v3.0/2026-02-20 08:46 -  
[DIR]v4.0/2026-03-19 09:28 -  
[TXT]HISTORY.txt2026-03-19 09:03 1.3K 
[TXT]LICENSE.txt2026-02-10 21:13 2.3K 
[TXT]README.html2026-03-19 10:19 4.9K 
[   ]v4.0.zip2026-03-19 10:15 35G 

TUD-L2B-EWH_UNC-GRACE

Welcome to the TU Delft Level-2B GRACE/GRACE-FO Equivalent Water Height (EWH) data repository. This archive provides versioned, uncertainty-aware gridded gravity products designed for hydrology, cryosphere, sea-level, and data-assimilation applications.

All datasets are derived from official GRACE and GRACE-FO Level-2 spherical harmonic solutions and are processed consistently to provide both signal estimates and a transparent, multi-component uncertainty decomposition.

This dataset provides gridded Equivalent Water Height (EWH), which are equivalent on land to Terrestrial Water Storage Anomalies (TWSA) from GRACE and GRACE-FO generated at TU Delft (“TUD”), filtered using the DDK{i} (i=2,...,7) decorrelation filter (Kusche et al., 2009) on a 0.5° × 0.5° global grid. Each file contains monthly fields from 2002–2020. All weighted mean and uncertainty components include gravity signal content from degree 2 to 60. Weights are computed as the normalised square inverses of open-ocean RMS using COST-G RL02.1 (Meyer, U. et al., 2025) monthly solutions as a benchmark. Coefficients C20 and C30 are already replaced using TN-14v3 (https://doi.org/10.1029/2019GL085488). The user can add the geocenter motion (TN-13) contribution (degree-1) separately, as well as remove prominent tidal components (S2, P1, S1, K1, and unmodelled R3), which can be found in the ancillary product TUD-L2B-EWH_CLIM-GRACE and for v4 in TUD-L2B-EWH_CLIM_CORR-GRACE.

The novelty in this product is the consolidation of multiple official GRACE Level-2 spherical harmonic solutions and their uncertainty propagation into a single multi-component uncertainty budget, which includes:
(1) the GIA trend (Bagge, M. et al. 2023),

(2) AOD1B (based on AOe07) (Shihora, L. et al. 2024),

(3) ensemble solution uncertainty (includes effects of parametrisation, and ocean tide models),

(4) filtering leakage (Dobslaw, H. et al. 2020), with finally

(5) degree-1 uncertainty (Swenson, S., D. Chambers, and J. Wahr, 2008).


Repository overview

Each version directory is fully self-contained and can be used independently. Users are strongly encouraged to explicitly reference the version number (e.g. v3.0 or v4.0) when using these data in scientific publications.