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Preliminary validation of SMOS products (levels 3 and 4)., , , , , , and . IGARSS, page 3170-3173. IEEE, (2010)Rain effects on ASCAT retrieved winds., , , , , , , and . IGARSS, page 2801-2804. IEEE, (2012)Overview of SMOS Level 2 Ocean Salinity processing and first results., , , , , , , , , and 14 other author(s). IGARSS, page 3146-3149. IEEE, (2010)SMOS measurements preliminary validation against modeled brightness temperatures and external-source salinity data., , , , , , , , , and 2 other author(s). IGARSS, page 3166-3169. IEEE, (2010)Derivation of an experimental satellite-based T-S diagram., , , , , , , , and . IGARSS, page 5760-5763. IEEE, (2012)Review of the CALIMAS Team Contributions to European Space Agency's Soil Moisture and Ocean Salinity Mission Calibration and Validation., , , , , , , , , and 25 other author(s). Remote Sensing, 4 (5): 1272-1309 (2012)Dominant Features of Global Surface Soil Moisture Variability Observed by the SMOS Satellite., , and . Remote Sensing, 11 (1): 95 (2019)Singularity Power Spectra: A Method to Assess Geophysical Consistency of Gridded Products - Application to Sea-Surface Salinity Remote Sensing Maps., , , , and . IEEE Trans. Geosci. Remote. Sens., 56 (9): 5525-5536 (2018)Seven Years of SMOS Sea Surface Salinity at High Latitudes: Variability in Arctic and Sub-Arctic Regions., , , , , , , , and . Remote. Sens., 10 (11): 1772 (2018)Synergy between Ocean Variables: Remotely Sensed Surface Temperature and Chlorophyll Concentration Coherence., , , and . Remote. Sens., 12 (7): 1153 (2020)