Publication Details

Category Text Publication
Reference Category Journals
DOI 10.5194/essd-18-4047-2026
Licence creative commons licence
Title (Primary) An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures for 2010–2024
Author Xing, Z.; Li, X.; Frappart, F.; De Lannoy, G.; Jagdhuber, T.; Peng, J. ORCID logo ; Fan, L.; Ma, H.; Karthikeyan, L.; Liu, X.; Wang, M.; Zhao, L.; Liu, Y.; Wigneron, J.-P.
Source Titel Earth System Science Data
Year 2026
Department RS
Volume 18
Issue 6
Page From 4047
Page To 4073
Language englisch
Topic T5 Future Landscapes
Data and Software links https://doi.org/10.5281/zenodo.17647385
Abstract The Soil Moisture and Ocean Salinity (SMOS) mission delivers the first multi-angular L-band observations for retrieving global soil moisture (SM) and vegetation optical depth (VOD), two critical variables for understanding terrestrial water and carbon cycles. However, the combined effects of non-identical fields of view and aliasing in multi-angular SMOS brightness temperature (TB) observations can introduce noise and biases when the TBs are averaged to a nominal incidence angle, as done in the SMOS L3 dataset, thereby degrading land parameter retrievals. To address this issue, an optimized SMOS TB dataset was initially produced at a fixed 40° incidence angle, consistent with the Soil Moisture Active Passive (SMAP) mission. We then developed the first SMOS mono-angular SM and VOD products designed to achieve performance comparable to SMAP and improved relative to conventional multi-angle SMOS retrievals. The 40° TB optimization was performed using the L-band Microwave Emission of the Biosphere (L-MEB) model, and the inversion relied on the SMAP-INRAE-BORDEAUX (SMAP-IB) algorithm, yielding a global 40° SMOS TB record and associated SM and VOD products for 2010–2024 at 25 km spatial resolution, collectively referred to as SMOS-IB. Results showed that the optimized 40° TB reached a performance level comparable to SMAP and improved relative to SMOS-L3, both in its sensitivity to in-situ SM from the International Soil Moisture Network (ISMN) and in the reduction of global pixel-scale noise. When multiple evaluation metrics are considered, the SMOS-IB SM and VOD data, benefiting from the use of the optimized TB as input and a newly optimized soil roughness (Hr) parameterization, showed improved performance compared with those derived from SMOS L3 40° TB or from the multi-angular SMOS products. The SMOS-IB TB, SM and VOD products can be used for L-band algorithm development and SMAP harmonization, global drought monitoring, and studies of vegetation water and biomass dynamics. SMOS-IB is publicly available at https://doi.org/10.5281/zenodo.17647385 (Xing et al., 2025).

Xing, Z., Li, X., Frappart, F., De Lannoy, G., Jagdhuber, T., Peng, J., Fan, L., Ma, H., Karthikeyan, L., Liu, X., Wang, M., Zhao, L., Liu, Y., Wigneron, J.-P. (2026):
An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures for 2010–2024
Earth Syst. Sci. Data 18 (6), 4047 - 4073
10.5194/essd-18-4047-2026