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dc.contributor.authorColliander, A.
dc.contributor.authorJackson, T.J.
dc.contributor.authorBindlish, R.
dc.contributor.authorChan, S.
dc.contributor.authorDas, N.
dc.contributor.authorKim, S.B.
dc.contributor.authorCosh, M.H.
dc.contributor.authorDunbar, R.S.
dc.contributor.authorDang, L.
dc.contributor.authorPashaian, L.
dc.contributor.authorAsanuma, J.
dc.contributor.authorAida, K.
dc.contributor.authorBerg, A.
dc.contributor.authorRowlandson, T.
dc.contributor.authorBosch, D.
dc.contributor.authorCaldwell, T.
dc.contributor.authorCaylor, K.
dc.contributor.authorGoodrich, D.
dc.contributor.authoral Jassar, H.
dc.contributor.authorLopez-Baeza, Ernesto
dc.contributor.authorMartínez Fernández, José 
dc.contributor.authorGonzález Zamora, Ángel 
dc.contributor.authorLivingston, S.
dc.contributor.authorMcNairn, H.
dc.contributor.authorPacheco, A.
dc.contributor.authorMoghaddam, M.
dc.contributor.authorMontzka, C.
dc.contributor.authorNotarnicola, C.
dc.contributor.authorNiedrist, G.
dc.contributor.authorPellarin, T.
dc.contributor.authorPrueger, J.
dc.contributor.authorPulliainen, J.
dc.contributor.authorRautiainen, K.
dc.contributor.authorRamos, J.
dc.contributor.authorSeyfried, M.
dc.contributor.authorStarks, P.
dc.contributor.authorSu, Z.
dc.contributor.authorZeng, Y.
dc.contributor.authorvan der Velde, R.
dc.contributor.authorThibeault, M.
dc.contributor.authorDorigo, W.
dc.contributor.authorVreugdenhil, M.
dc.contributor.authorWalker, J.P.
dc.contributor.authorWu, X.
dc.contributor.authorMonerris, A.
dc.contributor.authorO'Neill, P.E.
dc.contributor.authorEntekhabi, D.
dc.contributor.authorNjoku, E.G.
dc.contributor.authorYueh, S.
dc.date.accessioned2025-10-03T11:20:11Z
dc.date.available2025-10-03T11:20:11Z
dc.date.issued2017
dc.identifier.citationA. Colliander, T.J. Jackson, R. Bindlish, S. Chan, N. Das, S.B. Kim, M.H. Cosh, R.S. Dunbar, L. Dang, L. Pashaian, J. Asanuma, K. Aida, A. Berg, T. Rowlandson, D. Bosch, T. Caldwell, K. Caylor, D. Goodrich, H. al Jassar, E. Lopez-Baeza, J. Martínez-Fernández, A. González-Zamora, S. Livingston, H. McNairn, A. Pacheco, M. Moghaddam, C. Montzka, C. Notarnicola, G. Niedrist, T. Pellarin, J. Prueger, J. Pulliainen, K. Rautiainen, J. Ramos, M. Seyfried, P. Starks, Z. Su, Y. Zeng, R. van der Velde, M. Thibeault, W. Dorigo, M. Vreugdenhil, J.P. Walker, X. Wu, A. Monerris, P.E. O'Neill, D. Entekhabi, E.G. Njoku, S. Yueh, Validation of SMAP surface soil moisture products with core validation sites, Remote Sensing of Environment, Volume 191, 2017, Pages 215-231, ISSN 0034-4257, https://doi.org/10.1016/j.rse.2017.01.021. (https://www.sciencedirect.com/science/article/pii/S0034425717300329)es_ES
dc.identifier.issn0034-4257
dc.identifier.urihttp://hdl.handle.net/10366/167284
dc.description.abstract[EN]The NASA Soil Moisture Active Passive (SMAP) mission has utilized a set of core validation sites as the primary methodology in assessing the soil moisture retrieval algorithm performance. Those sites provide well-calibrated in situ soil moisture measurements within SMAP product grid pixels for diverse conditions and locations. The estimation of the average soil moisture within the SMAP product grid pixels based on in situ measurements is more reliable when location specific calibration of the sensors has been performed and there is adequate replication over the spatial domain, with an up-scaling function based on analysis using independent estimates of the soil moisture distribution. SMAP fulfilled these requirements through a collaborative Cal/Val Partner program. This paper presents the results from 34 candidate core validation sites for the first eleven months of the SMAP mission. As a result of the screening of the sites prior to the availability of SMAP data, out of the 34 candidate sites 18 sites fulfilled all the requirements at one of the resolution scales (at least). The rest of the sites are used as secondary information in algorithm evaluation. The results indicate that the SMAP radiometer-based soil moisture data product meets its expected performance of 0.04 m3/m3 volumetric soil moisture (unbiased root mean square error); the combined radar-radiometer product is close to its expected performance of 0.04 m3/m3, and the radar-based product meets its target accuracy of 0.06 m3/m3 (the lengths of the combined and radar-based products are truncated to about 10 weeks because of the SMAP radar failure). Upon completing the intensive Cal/Val phase of the mission the SMAP project will continue to enhance the products in the primary and extended geographic domains, in co-operation with the Cal/Val Partners, by continuing the comparisons over the existing core validation sites and inclusion of candidate sites that can address shortcomings.es_ES
dc.format.mimetypeapplication/pdf
dc.language.isoenges_ES
dc.publisherELSEVIERes_ES
dc.subjectSMAPes_ES
dc.subjectSoil Moisturees_ES
dc.subjectValidationes_ES
dc.titleValidation of SMAP surface soil moisture products with core validation siteses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1016/j.rse.2017.01.021es_ES
dc.identifier.doi10.1016/j.rse.2017.01.021
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.journal.titleRemote Sensing of Environmentes_ES
dc.volume.number191es_ES
dc.page.initial215es_ES
dc.page.final231es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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