Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/31705
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Analysis of waves observed by synthetic aperture radar across ocean fronts
Author(s): Shao, Weizeng
Jiang, Xingwei
Nunziata, Ferdinando
Marino, Armando
Yang, Zhehao
Zhang, Youguang
Corcione, Valeria
Contact Email: armando.marino@stir.ac.uk
Keywords: Wave
Ocean front
Synthetic aperture radar
Issue Date: Nov-2020
Date Deposited: 22-Sep-2020
Citation: Shao W, Jiang X, Nunziata F, Marino A, Yang Z, Zhang Y & Corcione V (2020) Analysis of waves observed by synthetic aperture radar across ocean fronts. Ocean Dynamics, 70 (11), p. 1397–1407. https://doi.org/10.1007/s10236-020-01403-2
Abstract: In this study, synthetic aperture radar (SAR) imaging of waves across ocean fronts was investigated using C-band Sentinel-1 VV-polarized SAR imagery collected over the Yangtze and the Zhujiang estuaries. The presence of ocean fronts in the study area was confirmed by collocated sea surface temperature (SST) data provided by the Advanced Very High Resolution Radiometer (AVHRR) and sea surface current information from the National Ocean Partnership Program (NOPP) based on the HYbrid Coordinate Ocean Model (HYCOM). The experimental results revealed that as the current speed increased, the cut-off wavelength (λc) increased as well. The effect of the increasing azimuth cut-off wavelength, however, was relatively weak in terms of variations of the normalized radar cross-section (NRCS), i.e., it was within 2 dB for λc ≤ 60 m. Hence, it was weaker than the NRCS variation related to SST. Larger NRCS variations (i.e., within 5 dB) occurred for λc values up to 120 m. In addition, the experimental results also demonstrated that the parameterized first-guess spectrum method (PFSM) wave retrieval performance was affected by ocean fronts. In particular, overestimations occurred when ocean fronts were present and λc was < 100 m
DOI Link: 10.1007/s10236-020-01403-2
Rights: This item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. This is a post-peer-review, pre-copyedit version of an article published in Ocean Dynamics. The final authenticated version is available online at: https://doi.org/10.1007/s10236-020-01403-2
Licence URL(s): https://storre.stir.ac.uk/STORREEndUserLicence.pdf

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