2015
DOI: 10.1016/j.asr.2014.12.011
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Mitigation of ECMWF–scatterometer wind biases in view of storm surge applications in the Adriatic Sea

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Cited by 15 publications
(13 citation statements)
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“…Kara et al (2009) compared, on a monthly basis, the QuikSCAT 25 km data with "analysis quality" NWP winds (A. Wallcraft, personal communication, 2014) coming from the NOGAPS dataset at 0.5°of resolution, in the Mediterranean Sea. Zecchetto et al (2015), proposed a new methodology for exploiting satellite-borne scatterometer wind observations to reduce the bias of numerical model prediction wind fields with respect to satellite-detected winds.…”
Section: Differences Between Model and Scatterometer Winds In The Adr...mentioning
confidence: 99%
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“…Kara et al (2009) compared, on a monthly basis, the QuikSCAT 25 km data with "analysis quality" NWP winds (A. Wallcraft, personal communication, 2014) coming from the NOGAPS dataset at 0.5°of resolution, in the Mediterranean Sea. Zecchetto et al (2015), proposed a new methodology for exploiting satellite-borne scatterometer wind observations to reduce the bias of numerical model prediction wind fields with respect to satellite-detected winds.…”
Section: Differences Between Model and Scatterometer Winds In The Adr...mentioning
confidence: 99%
“…De Biasio et al (2016, Bajo et al (2017) toke advantage of the methodology described in Zecchetto et al (2015), adapting a combined strategy, based on satellite scatterometry and satellite altimetry, in order to improve the prediction skills of a hydrodynamic model used for strom surge forecast in the Adriatic Sea and Venice, with positive results. In their study, the surface wind field was provided by the ECMWF numerical atmospheric model, scatterometer winds were derived from the SeaWinds scatterometer mounted on the American NASA QuikSCAT satellite, and from the ASCAT instruments onboard the European MetOP satellites.…”
Section: Differences Between Model and Scatterometer Winds In The Adr...mentioning
confidence: 99%
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“…The mitigation of the two bias in the model fields uses the bias registered in the preceding few days between scatterometer observations and model analyses, introducing them as counteracting terms in the definition of the mitigated model wind. This methodology has been first proposed and investigated in Zecchetto et al, 2015). The approach for the wind speed relies on the normalized bias Δw N (i, j) (Equation 3) as counteracting term, while that for the wind direction simply relies on Δθ(i,j) (Eq.…”
Section: Bias Mitigation Of the Atmospheric Model Wind Forcingmentioning
confidence: 99%
“…This goal was achieved in the framework of the eSurge-Venice projecta project funded by the Data User Element programme of the European Space Agency (ESA)by using satellite scatterometer wind and radar altimetry Total Water Level Envelope (TWLE: a quantity easily derived from the sea level anomaly) observations to increase the reliability and accuracy of the storm surge prediction in the Gulf of Venice. Satellite-borne scatterometer winds were used to mitigate the biases between the model and the measured winds with a methodology named wind-bias mitigation (Zecchetto, Della Valle, & De Biasio, 2015). Satellite altimetry brought instead a significant improvement of the sea level background field across the basin, through the assimilation of TWLE retrievals into the storm surge model (SSM) SHYFEM (online: http://www.ismar.cnr.it/shyfem), with a dual 4D-Var assimilation algorithm.…”
Section: Introductionmentioning
confidence: 99%