EGU26-14777, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-14777
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Thursday, 07 May, 10:45–12:30 (CEST), Display time Thursday, 07 May, 08:30–12:30
 
Hall X5, X5.103
GROSAT-GLOB: Synergetic Ground-Based and Satellite Retrievals for Global Surface Characterization and Validation
Smita Panda1, Pavel Litvinov1, Christian Matar1, Siyao Zhai1, Juan Gómez1, Zhen Liu1, Juan Carlos Antuña-Sánchez1, Anton Lopatin1, David Fuertes1, Oleg Dubovik2, Tatsiana Lapionak2, Benjamin Torres2, Christian Retscher3, Silvia Scifoni4, and Philippe Goryl4
Smita Panda et al.
  • 1GRASP SAS, Remote Sensing Developments, Lille, France
  • 2Laboratoire d'Optique Atmosphérique, CNRS/University of Lille, France
  • 3European Commission, DG CLIMA, Av. d’Auderghem 19, 1040 Bruxelles
  • 4ESA, ESRIN, Largo Galileo Galilei 1, 00044 Frascati (RM), Italy

Accurate characterization of land surface reflectance remains a fundamental challenge in satellite remote sensing, particularly over heterogeneous and bright surfaces where surface and atmospheric contributions are strongly coupled. Ground-based AERONET direct-sun and sky-radiance observations provide robust constraints on aerosol optical and microphysical properties, while satellite measurements provide spatially resolved information on surface reflection. In the GROSAT-GLOB approach, these complementary measurement types are combined to enable a more reliable separation of surface and atmospheric signals for surface characterization.

The GROSAT-GLOB approach implements a synergetic retrieval framework based on the GRASP inversion algorithm, integrating ground-based AERONET observations with collocated satellite radiance measurements. Aerosol optical and microphysical properties are primarily constrained by AERONET direct-sun and sky-radiance data, while satellite observations are used to retrieve surface reflectance. To ensure robustness and computational efficiency at the global scale, a two-step retrieval strategy is employed: aerosol microphysical properties are first retrieved by combining spatially aggregated (10–30 km) satellite observations with temporally collocated AERONET almucantar and direct-sun measurements, and are subsequently introduced as constrained a priori information to retrieve surface reflectance at the native satellite resolution using satellite radiances and direct-sun AOD measurements only.

The GROSAT-GLOB retrieval framework has been applied to multiple satellite sensors, including Sentinel-3 OLCI-A/B, Sentinel-5P/TROPOMI, PACE/HARP2, and MTG-FCI, demonstrating its general applicability across instruments with differing spatial resolutions, spectral coverage, and viewing geometries. The retrieved surface reflectance products are validated against independent reference datasets, including MODIS white-sky albedo, HYPERNET reflectance, and RadCalNet bottom-of-atmosphere reflectance, while aerosol retrievals are assessed against AERONET products. These intercomparisons provide a quantitative assessment of retrieval consistency and stability, supporting the use of GROSAT-GLOB products as a surface reference dataset for cross-sensor harmonization and satellite surface reflectance validation.

How to cite: Panda, S., Litvinov, P., Matar, C., Zhai, S., Gómez, J., Liu, Z., Antuña-Sánchez, J. C., Lopatin, A., Fuertes, D., Dubovik, O., Lapionak, T., Torres, B., Retscher, C., Scifoni, S., and Goryl, P.: GROSAT-GLOB: Synergetic Ground-Based and Satellite Retrievals for Global Surface Characterization and Validation, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-14777, https://doi.org/10.5194/egusphere-egu26-14777, 2026.