Kim, H.-J., A. J. Miller, J. McGowan and M. Carter, 2008:

Climate and coastal algal blooms in the Southern California Bight.


Progress in Oceanography, sub judice.

Abstract. Surface chlorophyll measured at the Scripps Pier in the Southern California Bight (SCB) for eighteen years (1983 - 2000) reveals that the spring bloom occurs with irregular timing and intensity each year, unlike sea-surface temperature (SST), which is dominated by a regular seasonal cycle. In the 1990's, the spring bloom occurred earlier in the year and with larger amplitudes compared to those of the 1980's. Seasonal anomalies of the chlorophyll have no significant correlation with local winds, offshore winds, or upwelling index anomalies. Consequently, classical coastal upwelling may not be the process that drives chlorophyll variations in the nearshore SCB. The annual mean Pier chlorophyll concentration exhibits a clear increasing trend with no concomitant trend evident in the Pier SST over these two decades. The interannual variations of the Pier SST and chlorophyll is not correlated with tropical El Nino or La Nina conditions over the entire observing period, but a few strong El Nino and La Nina events have significant impacts on the Pier data. The Pier chlorophyll is highly coherent at low frequencies (3-7 years) with nearby offshore in situ surface chlorophyll observations at the CalCOFI (California Cooperative Fisheries Investigations) station 93.27. Both the Pier and CalCOFI station 93.27 (12.5 km offshore) are on the continental shelf (water depth < 200m), but the Pier chlorophyll observations have magnitudes that are roughly one to two orders greater than the offshore surface chlorophyll observed by CalCOFI.

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