TY - GEN
T1 - The impact of thermal stratification and wind stress on sea surface features in SAR imagery
AU - Fujimura, Atsushi
AU - Matt, Silvia
AU - Soloviev, Alexander
AU - Maingot, Chris
AU - Rhee, Shin H.
PY - 2011
Y1 - 2011
N2 - We have conducted high-resolution numerical experiments with the computational fluid dynamics (CFD) software ANSYS FLUENT on the dynamics of centerline ship wakes and rain-formed plumes in the presence of wind stress. The ship wake model is initialized with the velocity field from numerical simulations using a model with a ship hull and propellers. We then apply wind stress perpendicular to the centerline wake. We simulate SAR images with a radar imaging algorithm using the surface velocity field produced by the CFD model. Results show ship wake asymmetry since the wind stress enhances flow convergence upwind of the centerline wake and reduces it on the downwind side. The results are qualitatively consistent with available SAR images. We added a near-surface thermal stratification (e.g., diurnal thermocline) to the model during initialization and investigated the impact on the ship wake hydrodynamics. Stratification appears to influence the spreading of the wake, while the circulation in the wake can bring colder water to the surface. For the plume simulation, we initialize the model with a low-density plume imitating randomly distributed rainfall. The plume structure also shows asymmetry relative to the wind direction in simulated radar images.
AB - We have conducted high-resolution numerical experiments with the computational fluid dynamics (CFD) software ANSYS FLUENT on the dynamics of centerline ship wakes and rain-formed plumes in the presence of wind stress. The ship wake model is initialized with the velocity field from numerical simulations using a model with a ship hull and propellers. We then apply wind stress perpendicular to the centerline wake. We simulate SAR images with a radar imaging algorithm using the surface velocity field produced by the CFD model. Results show ship wake asymmetry since the wind stress enhances flow convergence upwind of the centerline wake and reduces it on the downwind side. The results are qualitatively consistent with available SAR images. We added a near-surface thermal stratification (e.g., diurnal thermocline) to the model during initialization and investigated the impact on the ship wake hydrodynamics. Stratification appears to influence the spreading of the wake, while the circulation in the wake can bring colder water to the surface. For the plume simulation, we initialize the model with a low-density plume imitating randomly distributed rainfall. The plume structure also shows asymmetry relative to the wind direction in simulated radar images.
KW - computational fluid dynamics
KW - numerical simulation
KW - Ship wake
KW - synthetic aperture radar
UR - https://www.scopus.com/pages/publications/80955155000
UR - https://www.scopus.com/pages/publications/80955155000#tab=citedBy
U2 - 10.1109/IGARSS.2011.6049531
DO - 10.1109/IGARSS.2011.6049531
M3 - Conference contribution
AN - SCOPUS:80955155000
SN - 9781457710056
T3 - International Geoscience and Remote Sensing Symposium (IGARSS)
SP - 2037
EP - 2040
BT - 2011 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2011 - Proceedings
T2 - 2011 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2011
Y2 - 24 July 2011 through 29 July 2011
ER -