“…The non-linearity is accounted for by using the coefficients A i,j (i ≤ j ≤ n). The basic model of the CWAVE function, which has been successfully used to deal with SAR measurements collected by ERS [15], ENVISAT-ASAR [16], S-1 [17], and the Chinese Gaofen-3 [19], is given by:…”
Section: Methodsmentioning
confidence: 99%
“…Ocean wave retrieval algorithms include theoretical-based retrieval schemes, e.g., the "Max-Planck Institute" (MPI) [7][8][9], the Semi Parametric Retrieval Algorithm (SPRA) [10], the Partition Rescaling and Shift Algorithm (PARSA) [11], and the Parameterized First-guess Spectrum Method (PFSM) [12][13][14], as well as empirical models, e.g., CWAVE_ERS [15], CWAVE_ENVI [16], CWAVE_S1 [17], CSAR_WAVE [18,19], and QPCWAVE_GF3 [20]. All these algorithms have been developed to exploit SAR measurements collected at low and moderate sea states, due to the lack of SAR datasets collected at high sea state conditions.…”
In this study, an empirical algorithm is proposed to retrieve significant wave height (SWH) from dual-polarization Sentinel-1 (S-1) synthetic aperture radar (SAR) imagery collected under cyclonic conditions. The retrieval scheme is based on the well-known CWAVE empirical function that is here updated to deal with multi-polarization S-1 SAR measurements collected using the interferometric wide (IW) and the Extra Wide-Swath (EW) imaging modes, under cyclonic conditions. First, a training dataset that consists of six S-1 SAR images collected under cyclonic conditions is exploited to both tune the retrieval function and to check the soundness of the retrievals against the co-located WAVEWATCH-III (WW3) numerical simulations. The comparison of simulation from the WW3 model and measurements from altimeter Jason-2 shows a 0.29m root mean square error (RMSE) of significant wave height (SWH). Then, a testing data-set that consists of two S-1 SAR images is exploited to provide a preliminary validation. The results, verified against both WW3 and European Centre for Medium-Range Weather Forecasts (ECMWF) data, show the soundness of the herein approach.
“…The non-linearity is accounted for by using the coefficients A i,j (i ≤ j ≤ n). The basic model of the CWAVE function, which has been successfully used to deal with SAR measurements collected by ERS [15], ENVISAT-ASAR [16], S-1 [17], and the Chinese Gaofen-3 [19], is given by:…”
Section: Methodsmentioning
confidence: 99%
“…Ocean wave retrieval algorithms include theoretical-based retrieval schemes, e.g., the "Max-Planck Institute" (MPI) [7][8][9], the Semi Parametric Retrieval Algorithm (SPRA) [10], the Partition Rescaling and Shift Algorithm (PARSA) [11], and the Parameterized First-guess Spectrum Method (PFSM) [12][13][14], as well as empirical models, e.g., CWAVE_ERS [15], CWAVE_ENVI [16], CWAVE_S1 [17], CSAR_WAVE [18,19], and QPCWAVE_GF3 [20]. All these algorithms have been developed to exploit SAR measurements collected at low and moderate sea states, due to the lack of SAR datasets collected at high sea state conditions.…”
In this study, an empirical algorithm is proposed to retrieve significant wave height (SWH) from dual-polarization Sentinel-1 (S-1) synthetic aperture radar (SAR) imagery collected under cyclonic conditions. The retrieval scheme is based on the well-known CWAVE empirical function that is here updated to deal with multi-polarization S-1 SAR measurements collected using the interferometric wide (IW) and the Extra Wide-Swath (EW) imaging modes, under cyclonic conditions. First, a training dataset that consists of six S-1 SAR images collected under cyclonic conditions is exploited to both tune the retrieval function and to check the soundness of the retrievals against the co-located WAVEWATCH-III (WW3) numerical simulations. The comparison of simulation from the WW3 model and measurements from altimeter Jason-2 shows a 0.29m root mean square error (RMSE) of significant wave height (SWH). Then, a testing data-set that consists of two S-1 SAR images is exploited to provide a preliminary validation. The results, verified against both WW3 and European Centre for Medium-Range Weather Forecasts (ECMWF) data, show the soundness of the herein approach.
“…It can be seen from our recent study (Sheng et al 2018) that the RMSE of the SWH is about 0.52m for co-polarization GF-3 SAR imaging mode acquired in QPS-I/II when retrieval results are compared with the measurements from altimeter Jason-2. It was also found that CSAR_WAVE2 has a better performance of wave retrieval for GF-3 SAR than the analysis results achieved when using the other empirical algorithms proposed in Wang et al (2012), Ren et al (2015) and Grieco et al (2016).…”
Section: Csar_wave2mentioning
confidence: 97%
“…In addition, several recent studies have developed algorithms to retrieve SWH through the cutoff wavelength at C-band for R-2 (Ren et al 2015), S-1 SAR (Shao et al 2016;Grieco et al 2016;Stopa and Mouche, 2017). In our recent study, an empirical algorithm is exploited for GF-3 SAR in co-polarization, named CSAR_WAVE2 (Sheng et al 2018). CSAR_WAVE2 employs the basic formulation of the CWAVE model, in which the coefficients are tuned through 1523 GF-3 SAR QPS-I/II mode images with collocated European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis SWH data at 0.125 grids.…”
Our work describes the accuracy of the Chinese quad-polarization Gaofen-3 (GF-3) synthetic aperture radar (SAR) wave mode data for wave retrieval and provides guidance for operational applications of GF-3 SAR. In this study, we have evaluated the accuracy of SAR-derived significant wave height (SWH) from 10514 GF-3 SAR images with visible wave streak acquired in wave mode by using the existing wave retrieval algorithms, e.g., the theoretical-based algorithm parameterized first-guess spectrum method (PFSM), the empirical algorithm CSAR_WAVE2 for VV-polarization, and the algorithm for quad-polarization (Q-P). The retrieved SWHs are compared with the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis field at 0.125° grids. The root mean square error (RMSE) of SWH is 0.57m by using CSAR_WAVE2 is achieved, which is less than the analysis results achieved by using algorithm PFSM and Q-P. The statistical analysis also indicates that wind speed has little impact on bias with increasing wind speed.However, the retrieval tends to overestimate when SWH is smaller than 2.5m and
“…Figure 1 shows the footprints of available GF-3 images for this study. For calculating the NRCS from VV- and HH-polarization GF-3 SAR intensity images, the digital number (DN) is converted into NRCS following Sheng et al (2018):…”
In this study, a re-tuned algorithm based on the geophysical model function (GMF) C-SARMOD2 is proposed to retrieve wind speed from Synthetic Aperture Radar (SAR) imagery collected by the Chinese C-band Gaofen-3 (GF-3) SAR. More than 10,000 Vertical-Vertical (VV) and Horizontal-Horizontal (HH) polarization GF-3 images acquired in quad-polarization stripmap (QPS) and wave (WV) modes have been collected during the last three years, in which wind patterns are observed over open seas with incidence angles ranging from 18° to 52°. These images, collocated with wind vectors from the European Centre for Medium-Range Weather Forecast (ECMWF) reanalysis at 0.125° resolution, are used to re-tune the C-SARMOD2 algorithm to specialize it for the GF-3 SAR (CSARMOD-GF). In particular, the CSARMOD-GF performs differently from the C-SARMOD2 at low-to-moderate incidence angles smaller than about 34°. Comparisons with wind speed data from the Advanced Scatterometer (ASCAT), Chinese Haiyang-2B (HY-2B) and buoys from the National Data Buoy Center (NDBC) show that the root-mean-square error (RMSE) of the retrieved wind speed is approximately 1.8 m/s. Additionally, the CSARMOD-GF algorithm outperforms three state-of-the-art methods -C-SARMOD, C-SARMOD2, and CMOD7 -that, when applied to GF-3 SAR imagery, generating a RMSE of approximately 2.0-2.4 m/s.
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