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Palabras clave – provistas por la editorial

soil moisture; root zone; SMAP; SMOS; MODIS; climatology; trends; signal decomposition; interferometric radiometry; image reconstruction; error correction; surface currents; mediterranean sea; satellite altimetry; sea surface temperature; sea surface salinity; BEC SMOS products; Mediterranean Sea; Algerian Basin; ABACUS gliders; microwave remote sensing; CIMR; copernicus marine service; satellite observations; tidal currents; internal tides; data assimilation; 4D-Var; Congo River plume; satellite salinity; Angola Basin; ROMS; moisture variability; temporal dynamics; moisture patterns; spatial disaggregation; Soil Moisture Active Passive (SMAP); Soil Moisture and Ocean Salinity (SMOS); REMEDHUS; L-band radiometry; Soil Moisture and Ocean Salinity (SMOS) mission; sea ice thickness; retrieval model validation; upward looking sonar; Arctic; altimetry; surface quasi-geostrophic equations; remote sensing; ocean color; data fusion; data merging; physical oceanography; singularity analysis; faraday rotation angle (FRA); vertical total electron content (VTEC); L-band; radiometry; Interferometry; ocean salinity (SMOS); calibration; reprocessing; BEC; oceanography; cryosphere; processing; sensor calibration