On the contrary, during SWD winds, a smaller level of TKE is responsible for small-size stress spheroid formation. The average volume of the corresponding Reynolds stress spheroids during the LWD is 13% larger than that of during SWD wind....
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Wave measurements from an acoustic Doppler current profiler (ADCP) sensor moored in 17 m depth (datum), and operating during a rather stormy period, were used to model comparisons. The comparison showed that no significant differences in the results were found between the two wind field ...
The interaction between a volatile salinity gradient and along-estuary wind forcing is found to cause temporary inversions of the estuarine circulation. Despite the highly dynamic conditions, the applicability of recent theories for isohaline mixing, using the framework of Total Exchange Flow, and the...
J. A. JiménezD. MorónA. SánchezArcilllaJ. GuillénA. PalanquesGracia, V., Moro´n, D., Jime´nez, J. A., Guille´n, J., Palanques, A., and Sanchez-Arcilla, A.: Near-bottom transport seaward of the surf zone under storms: On the role of currents, wind and in- fra...
Wave contribution was only relevant during the peak of the storm and when wind decreases in intensity and opposite to the mean current being the only agent that introduces sediment into the system. Low frequency oscillatory motions are strongly correlated with high frequency ones indicating a wave ...
We used a normalized SB component (SBCN = SBC/U) to detect SB days. A negative value of SBCN (~−1) indicates the easterly wind (SWD) and a positive value (~1) matches the westerly wind (LWD). In this study, the sonic measurement of zonal, meridional, and vertical velocity ...