Current temporal asymmetry and the role of tides: Nan-Wan Bay vs. the Gulf of Elat

Yosef Ashkenazy, Ben-Gurion University of the Negev Midreshet, Sde Boker, Israel, Erick Fredj, The Jerusalem College of Technology, Jerusalem, Israel, Hezi Gildor, Hebrew University of Jerusalem, Jerusalem, Israel, Gwo-Ching Gong, National Taiwan Ocean University, Institute of Marine Environment and Ecology, Keelung, Taiwan, Hung-Jen Lee, National Taiwan Ocean University, Department of Marine Environmental Informatics, Keelung, Taiwan and Chau-Ron Wu, National Taiwan Normal University, Department of Earth Sciences, Taipei, Taiwan
Abstract:
Nan-Wan Bay in Taiwan and the Gulf of Elat in Israel are two different coastal environments and as such are expected to have different statistical properties of their currents. While the Nan-Wan Bay is shallow, has three open boundaries, and directly connected to the open ocean, the Gulf of Elat is deep, semi-enclosed, and connected to the Red Sea via the Straits of Tiran. High temporal (less or equal one hour) and spatial (less or equal one km) surface currents have been measured continuously for more than a year in both environments using Coastal Radars (CODARs) that cover a domain of roughly 10×10 kms. These measurements show that the currents in Nan-Wan Bay are much stronger than those in the Gulf of Elat and that the mean current field in Nan-Wan Bay exhibits cyclonic circulation, which is stronger in the summer; in the Gulf of Elat the mean current field is directed to south and is stronger during the summer. We have compared the statistical properties of the CODAR current speeds in both environments and found that both exhibit large spatial and seasonal variations in the shape parameter of the Weibull distribution. However, we have found fundamental and significant differences when comparing the temporal asymmetry of the current speed (i.e., the ratio between the time during which the current speed is increasing to the total time). While the Nan-Wan Bay currents are significantly asymmetric, those of the Gulf of Elat are not significantly asymmetric. We then extracted the tidal component of the Nan-Wan Bay currents and found that it is strongly asymmetric while the asymmetry of tidally-filtered currents is much weaker. We thus conclude that the temporal asymmetry of the Nan-Wan Bay currents reported here is due to the strong tides in the region. We show that the asymmetry ratio in the Nan-Wan Bay is varied spatially and seasonally: (i) currents increase rapidly and decay slowly in the northern part of the domain and vice versa in the southern part, and that (ii) the asymmetry is stronger during summer.
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