In the last decades, advances in weather forecasting have been rapid, benefiting numerous social and environmental areas already facing global warming challenges. These advances resulted from more and better observations, mainly due to space-based remote sensing (Schmetz & Menzel, 2015), improved numerical weather prediction (NWP) models, its integration through enhanced assimilation methods, and other technological advances (Alley et al., 2019;Bauer et al., 2015). However, the water vapor dynamics, one of the key components to understanding weather and climate change behavior, remains a major challenge for forecast models (Bannister et al., 2020;Sherwood et al., 2010). Improving the moisture accuracy of NWP models requires information regarding the distribution of water vapor in the atmosphere at meso-and micro-scales. In addition, a better water vapor forecast will improve the prediction of extreme events that are getting even more relevant due to climate change (Schewe et al., 2019).Interferometric synthetic aperture radar (InSAR) is the only technique available that can provide maps of Precipitation Water Vapor (PWV) over large areas at high spatial resolution (5 × 20 m 2 nominal resolution in Interferometric Wide-Swath (I.W.) mode; Mateus et al., 2017Mateus et al., , 2020. Previous studies have demonstrated that InSAR-derived PWV data can improve the representation of moisture in numerical models and its spatial distribution, resulting in better precipitation predictions. For example, Pichelli et al. (2015) were the first to assimilate InSAR PWV data, acquired by the Environmental Satellite (ENVISAT) over Rome, Italy, using the mesoscale weather prediction model MM5 and the 3D Variational (3DVAR) scheme. They improved the forecast of weak to moderate precipitation (<15 mm/3 hr) and obtained a better description of the local precipitation event considered. Mateus et al. ( 2016) followed up with a similar study using data acquired over Lisbon, Portugal, and the Weather Research and Forecasting model (WRF), showing an improvement in the light precipitation forecast up to 9 hr after the assimilation time. Mateus et al. (2018) demonstrated the value of InSAR data improving the forecast of two successive deep convective storms (approximately 12 hr apart), using data acquired by Sentinel-1 mission over Adra, Spain. Lagasio et al. (2019) andPierdicca et al. (2020) assimilated Sentinel, and Global Navigation Satellite System (GNSS) derived data into the WRF model initialized by the Global Forecast System (GFS), improving the forecast skill of two severe precipitation events that occurred in Italy. Miranda et al. (2019) were the first to assimilate a large sequence of Sentinel-1 data acquired over the Appalachian Mountains in a time window