2000
DOI: 10.1109/36.851772
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On the assimilation of Ku-band scatterometer winds for weather analysis and forecasting

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Cited by 37 publications
(26 citation statements)
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“…To avoid the bias inherent to such binning process when calculations are performed versus one wind reference (Freilich, 1997), the difference between QuikSCAT and ASCAT winds (in this order) is estimated according to QuikSCAT and ASCAT wind speed 1 m/s bins. Therefore, the difference is significant if the two calculations provide similar trends.…”
Section: Data Coherencymentioning
confidence: 99%
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“…To avoid the bias inherent to such binning process when calculations are performed versus one wind reference (Freilich, 1997), the difference between QuikSCAT and ASCAT winds (in this order) is estimated according to QuikSCAT and ASCAT wind speed 1 m/s bins. Therefore, the difference is significant if the two calculations provide similar trends.…”
Section: Data Coherencymentioning
confidence: 99%
“…They were successfully used within assimilation process in numerical weather prediction models (e.g. Figa et al, 2000). Numerous studies demonstrated the positive impact of scatterometer wind retrievals in predicting and describing tropical cyclones (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Considering that conventional wind-only retrieval does not explicitly account for the sensitivity of backscatter measurements to rain, rain contamination introduces errors to retrieved wind velocities, particularly at high incidence angles. In order to prevent adverse rain impact on retrieved winds, quality control (QC) methods [4]- [6] are used to discard raincontaminated measurements-a process that causes the loss of Manuscript coverage. Considering that the successor of ESCAT, which is the advanced scatterometer instrument (ASCAT) on the MetOp-A satellite, has a higher incidence angle coverage than ESCAT, wind retrieval from ASCAT measurements is expected to be more sensitive to rain.…”
Section: Introductionmentioning
confidence: 99%
“…The use of satellite-derived high-spatial-resolution SSW for validation and assimilation in atmospheric circulation models is another important challenge. The current literature includes several examples of scatterometer-derived SSW assimilation in numerical weather prediction (NWP) models (Figa and Stoffelen 2000;Singh, Kumar, and Pal 2012) but, to our knowledge, the assimilation of synthetic aperture radar (SAR)-derived SSW in NWP models and the validation of NWP models by means of sensitivity studies are described in Section 3 and the conclusions are given in the final section (Section 6). For the sake of simplicity and clarity we will refer to the XMOD2 GMF developed by Li and Lehner (2014) as XMOD2-DLR, while XMOD2-ASI denotes the GMF developed by Nirchio and Venafra (2013).…”
Section: Introductionmentioning
confidence: 99%