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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)Rain Effects on ASCAT-Retrieved Winds: Toward an Improved Quality Control., , , , , , and . IEEE Trans. Geosci. Remote. Sens., 50 (7): 2495-2506 (2012)Empirical Characterization of the SMOS Brightness Temperature Bias and Uncertainty for Improving Sea Surface Salinity Retrieval., , , , , , , , , and . IEEE J Sel. Topics in Appl. Earth Observ. and Remote Sensing, 12 (7): 2486-2503 (2019)New SMOS salinity products at CP34-BEC in Barcelona., , , , , , , , , and 1 other author(s). IGARSS, page 4005-4007. IEEE, (2016)Empirical Characterization of The Smos Brightness Temperature Bias and Uncertainty for Improving Sea Surface Salinity., , , , , , , , and . IGARSS, page 1515-1518. IEEE, (2018)On the enhancement of the SMOS salinity products at CP34-BEC: From L0 to L4., , , , , and . IGARSS, page 296-298. IEEE, (2016)