Cross-shelf transport at Huntington Beach. Implications for the fate of sewage discharged through an offshore ocean outfall.
In this study, we evaluate the potential for internal tides to transport wastewater effluent from the Orange County Sanitation District (OCSD) ocean outfall toward Huntington Beach. Results of plume tracking studies show that OCSD effluent occasionally moves shoreward into water less than 20 m deep. Analyses of current and temperature observations indicate cold water is regularly advected cross-shelf, in to and out of the nearshore, at both semi-diurnal and diurnal frequencies. Isotherms typically associated with the waste field near the outfall are observed just outside the Huntington Beach surf zone, where the total depth is less than 6 m, highlighting the extent of the cross-shelf transport. This advection is attributed to a mode 1 internal motion, or internal tide. On the basis of the analyses presented here, the OCSD plume cannot be ruled out as a contributor to poor bathing-water quality at Huntington Beach.
Boehm
Alexandria B
AB
Department of Chemical Engineering and Materials Science, Henri Samueli School of Engineering, University of California-Irvine, 92697, USA.
Sanders
Brett F
BF
Winant
Clinton D
CD
D002140:California; D004784:Environmental Monitoring; D006801:Humans; D008962:Models, Theoretical; D011634:Public Health; D011998:Recreation; D012722:Sewage; D013696:Temperature; D014872:Water Movements; D014873:Water Pollutants / Q000032:analysis*; D014881:Water Supply
D012722:Sewage; D014873:Water Pollutants