FISHERY BULLETIN: VOL. 75, NO. 4 



Bakun (1973) pointed out that winters of extreme 

 shoreward convergence of wind-drifted surface 

 waters (negative index anomaly) should cause 

 the density structure to be depressed toward the 

 coast and should accelerate northward flow or de- 

 celerate southward flow. "Either situation would 

 favor an anomalous warm advection," according to 

 Bakun. 



ACKNOWLEDGMENTS 



The sampling program for this study was 

 started by Jefferson J. Gonor and William G. 

 Pearcy who graciously allowed us to participate. 

 R. Gregory Lough, Peter Rothlisberg, and others 

 helped with the sampling. William Gilbert pro- 

 vided the wind data and drafted Figure 4. The 

 manuscript was greatly improved by Lawrence F. 

 Small. The work was supported by NOAA, U.S. 

 Department of Commerce, Sea Grant Institu- 

 tional Grant No. 04-3-158-4. 



LITERATURE CITED 



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