**Miriam Pablos \*, Ángel González-Zamora, Nilda Sánchez and José Martínez-Fernández**

Instituto Hispanoluso de Investigaciones Agrarias (CIALE), University of Salamanca, Duero 12,

37185 Villamayor, Spain; aglezzamora@usal.es (A.G.-Z.); nilda@usal.es (N.S.); jmf@usal.es (J.M.-F.)

**\*** Correspondence: mpablos@usal.es; Tel.: +34-923-294-500

Received: 29 May 2018; Accepted: 18 June 2018; Published: 21 June 2018

**Abstract:** In this study, six satellite-based root zone soil moisture (RZSM) estimates from March 2015 to December 2016 were evaluated both temporally and spatially. The first two were the Soil Moisture Active Passive (SMAP) and the Soil Moisture and Ocean Salinity (SMOS) L4 RZSM products. The other four were obtained through the Soil Water Index (SWI) approach, which embedded surface soil moisture (SSM). The SMOS-Barcelona Expert Center (BEC) L4 SSM product and the apparent thermal inertia (ATI)-derived SSM from the Moderate Resolution Imaging Spectroradiometer (MODIS) data were used as SSM datasets. In the temporal analysis, the RZSM estimates were compared to in situ RZSM from 14 stations of the Soil Moisture Measurements Station Network of the University of Salamanca (REMEDHUS). Regarding the spatial assessment, the resulting RZSM maps of the Iberian Peninsula were compared between them. All RZSM values followed the temporal evolution of the ground-based measurements well, although SMOS and MODIS showed underestimation while SMAP displayed overestimation. The good results obtained from MODIS ATI are notable, notwithstanding they were not estimated through microwave radiometry. A very high agreement was found in terms of spatial patterns for the whole Iberian Peninsula except for the extreme north area, which is dominated by high mountains and dense forests.

**Keywords:** soil moisture; root zone; SMAP; SMOS; MODIS
