2016
DOI: 10.1109/tgrs.2016.2599219
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Three-Dimensional Variational Assimilation of InSAR PWV Using the WRFDA Model

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Cited by 36 publications
(29 citation statements)
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“…While some investigations on the assimilation in NWP models of low resolution (tens of km) EO derived products (e.g., soil moisture extracted from the Soil Moisture and Ocean Salinity mission data), are available in the literature [7], few studies were conducted on the ingestion of HR EO products. Only a few papers on the assimilation of water vapour maps derived from InSAR data [8][9][10] and one paper on the ingestion of SAR derived soil moisture maps [11] are available in the literature. These works consider a small spatial domain [8,10] or grid spacing at the cloud-permitting limit (3 km [9]).…”
Section: Introductionmentioning
confidence: 99%
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“…While some investigations on the assimilation in NWP models of low resolution (tens of km) EO derived products (e.g., soil moisture extracted from the Soil Moisture and Ocean Salinity mission data), are available in the literature [7], few studies were conducted on the ingestion of HR EO products. Only a few papers on the assimilation of water vapour maps derived from InSAR data [8][9][10] and one paper on the ingestion of SAR derived soil moisture maps [11] are available in the literature. These works consider a small spatial domain [8,10] or grid spacing at the cloud-permitting limit (3 km [9]).…”
Section: Introductionmentioning
confidence: 99%
“…Only a few papers on the assimilation of water vapour maps derived from InSAR data [8][9][10] and one paper on the ingestion of SAR derived soil moisture maps [11] are available in the literature. These works consider a small spatial domain [8,10] or grid spacing at the cloud-permitting limit (3 km [9]). Hence, to the best of the authors knowledge, there is currently no investigation that combines a big domain with a very high grid spacing (of the order of 1 km, in the cloud resolving range) and considers more than only one EO derived variable.…”
Section: Introductionmentioning
confidence: 99%
“…Pichelli et al () found improvements in hindcasting weak to moderate precipitation (<15 mm/3 hr) in a three‐dimensional variational (3D‐Var) data assimilation of InSAR‐PWV maps using the mesoscale weather prediction model Fifth‐Generation Penn State/National Center for Atmospheric Research Mesoscale Model (MM5) and ENVISAT‐Advanced Synthetic Aperture Radar (ASAR) data over the city of Rome, Italy. Mateus et al () showed a significant improvement in the atmospheric moisture content and on the formation of light precipitation up to 9 hr after the assimilation time in a 3D‐Var data assimilation experiment using InSAR‐PWV maps, estimated from the ENVISAT‐ASAR data, and the Weather Research and Forecast (WRF) model over Lisbon, Portugal. Mateus et al () showed that in a case with two successive deep convection storms, which could be both well forecasted only after InSAR data assimilation, using two PWV maps estimated from new generation SAR images obtained by Sentinel‐1 A over Adra, Spain, with the 3D‐Var method and the WRF model.…”
Section: Introductionmentioning
confidence: 99%
“…This approach requires the simultaneous acquisition of the external data and of the SAR data, which is not always feasible. Mateus et al (2016) suggested the use of a reanalysis product, opportunely oversampled over an NWP model grid, to reach a finer spatial resolution. Mateus et al (2018) tried instead to obtain a relatively fine resolution master map with an NWP model run.…”
Section: Introductionmentioning
confidence: 99%