TY - JOUR
T1 - Impact of model resolution on radar imaging of underwater sand waves
AU - Yu, Peng
AU - Zhong, Xiaojing
AU - Zhou, Yunxuan
N1 - Publisher Copyright:
© Coastal Education and Research Foundation, Inc. 2018.
PY - 2018/1/1
Y1 - 2018/1/1
N2 - Yu, P.; Zhong, X., and Zhou, Y., 2018. Impact of model resolution on radar imaging of underwater sand waves. Radar sensors are capable of imaging varying sea-surface roughness attributable to divergent and convergent current flow over underwater sand waves. This manifestation can be simulated and explored through a flow model combined with a radar-imaging model by explaining the interaction between bathymetry, currents, and surface waves. Accuracy of numerical models is usually limited by grid resolution; however, a lack of studies is present regarding the influence of grid resolution on the combined flow and radar-imaging model, which can determine the research scale of oceanic phenomena based on radar-imaging theory. To examine the role of grid size on imaging of distinct scales of sand ridges and to ignore other sources of surface-roughness variations in coastal areas, the authors designed an idealized flow model integrated with a radar-imaging model with different resolution. The results indicate that high-resolution synthetic aperture radar (SAR) images may be possible to detect bottom features smaller than 100 m. As the increasing grid resolution, surface-roughness variations can gradually reach a stable phase, indicating that the grid spacing should be elaborately selected according to the scale and complexity of underwater topography to fully present performance of the two-dimensional combined model. This model offers a reference to study the application of a radar-imaging mechanism or to analyze morphological changes based on SAR images and the combined system in coastal areas for future work.
AB - Yu, P.; Zhong, X., and Zhou, Y., 2018. Impact of model resolution on radar imaging of underwater sand waves. Radar sensors are capable of imaging varying sea-surface roughness attributable to divergent and convergent current flow over underwater sand waves. This manifestation can be simulated and explored through a flow model combined with a radar-imaging model by explaining the interaction between bathymetry, currents, and surface waves. Accuracy of numerical models is usually limited by grid resolution; however, a lack of studies is present regarding the influence of grid resolution on the combined flow and radar-imaging model, which can determine the research scale of oceanic phenomena based on radar-imaging theory. To examine the role of grid size on imaging of distinct scales of sand ridges and to ignore other sources of surface-roughness variations in coastal areas, the authors designed an idealized flow model integrated with a radar-imaging model with different resolution. The results indicate that high-resolution synthetic aperture radar (SAR) images may be possible to detect bottom features smaller than 100 m. As the increasing grid resolution, surface-roughness variations can gradually reach a stable phase, indicating that the grid spacing should be elaborately selected according to the scale and complexity of underwater topography to fully present performance of the two-dimensional combined model. This model offers a reference to study the application of a radar-imaging mechanism or to analyze morphological changes based on SAR images and the combined system in coastal areas for future work.
KW - Bathymetry
KW - TELEMAC
KW - grid resolution
KW - synthetic aperture radar (SAR) imaging
UR - https://www.scopus.com/pages/publications/85042318404
U2 - 10.2112/JCOASTRES-D-16-00227.1
DO - 10.2112/JCOASTRES-D-16-00227.1
M3 - 文章
AN - SCOPUS:85042318404
SN - 0749-0208
VL - 34
SP - 114
EP - 121
JO - Journal of Coastal Research
JF - Journal of Coastal Research
IS - 1
ER -