Wind relaxations and poleward flow events in a coastal upwelling system on the central California coast

• Published in: Journal of Geophysical Research. B. Solid Earth 2009-11, Vol.114 (C11), p.n/a
• Main Authors: Melton, Christopher, Washburn, Libe, Gotschalk, Chris
• Format: Article
• Language: English
• Subjects: Coastal; Coastal environments; Earth sciences; Earth, ocean, space; Exact sciences and technology; Geophysics; Marine; Moorings; oceanography; physical; Physical oceanography; Ports; Sea level; Statistics; Temperature distribution; Time series; Upwelling; Wind
• ISSN: 0148-0227; 2169-9275; 2156-2202; 2169-9291
• DOI: 10.1029/2009JC005397

When upwelling favorable winds weaken or relax in coastal upwelling systems, prevailing equatorward currents often weaken and then reverse to form propagating poleward currents. Here the statistics of wind relaxations and poleward flow events along the south central California coast are derived using meteorological and oceanographic times series during 2000–2006. Over the 7‐year record, 169 wind relaxations were observed (about 1 every 2 weeks) and 127 of these were followed by poleward flow events. Thermistor moorings and current profilers along the 15 m isobath at Alegria, Point Arguello, Point Purisima, and Point Sal recorded the poleward flows. The poleward flows propagate northward at 10–30 km d−1 and appear as sequential temperature increases at the moorings. Wind relaxations occur throughout the year but are most frequent in September and least frequent in April when upwelling winds are strong and persistent. Poleward flows follow wind relaxations frequently during May through November and rarely in December and January. Sea level differences between Santa Monica and Port San Luis, California, decreased as winds relaxed, consistent with forcing by alongshore pressure gradients. Temperature distributions at Point Arguello, Point Purisima, and Point Sal were skewed toward higher values because of the poleward flows. The alongshore distance traveled by the poleward flows increased with duration of the wind relaxations and magnitudes of alongshore temperature and sea level differences prior to the relaxations.