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2008 Annual Monitoring Report (pdf 10.9MB) - Bolsa Chica ...

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<strong>Bolsa</strong> <strong>Chica</strong> Lowlands Restoration <strong>Monitoring</strong><br />

<strong>2008</strong> <strong>Annual</strong> <strong>Report</strong><br />

from July 1-16 and generally ranged between 5 and 20 NTU. Dissolved oxygen data at Station 1 were<br />

unacceptable, but deployment, mid-deployment, and retrieval readings taken with a separate<br />

instrument recorded DO levels ranging between 5.6 and 7.6 mg/L. Dissolved oxygen at Station 2 for<br />

the 30-day period ranged from 4.1 to 9.4 mg/L, with a mean of 7.2 mg/L.<br />

Additional spot water quality readings taken at the same stations during concurrent fisheries<br />

monitoring were presented in the fisheries monitoring section of this report.<br />

Discussion<br />

The water quality conditions observed in the FTB during the last three quarters of Year 2 monitoring<br />

show the tidal marine influence that exists in the basin, reflecting the daily and monthly tidal<br />

fluctuations seen in the open ocean. All parameters were well within acceptable ranges to support the<br />

developing fish, invertebrate, and vegetation communities, and are indicative of a well-flushed marine<br />

environment. On-going physical monitoring of the condition of the inlet and the flood shoal is<br />

important to ensure proper circulation of the basin and maintenance of good water quality.<br />

The lack of usable paired temperature data at both stations makes comparisons difficult, but reviewing<br />

the limited data available in conjunction with water quality measurements taken at the time of the<br />

fisheries monitoring allows for some assessment. In the April and July months, there was a south to<br />

north gradient of increasing water temperature. During warmer months the slow-circulating waters in<br />

at the northern end of the basin tended to have higher temperatures because of increased solar heating.<br />

The better circulated waters of the southern portion of the basin were more influenced by cooler<br />

oceanic water, maintaining lower temperatures during the warmer months. Very little difference in<br />

temperature was seen between the two stations during the January sampling.<br />

Monthly average sea surface temperature data were obtained from the Coastal Data Information<br />

Program (CDIP) (http://cdip.ucsd.edu/) for the closest station: 092 San Pedro (offshore of LA/LB<br />

Harbors, 10 kilometers south of Point Fermin). The mean monthly sea surface temperature in January<br />

<strong>2008</strong> was 13.7 °C, while it was an average of 13.4 °C at both Station 1 and 2 in the FTB. In April<br />

<strong>2008</strong> the sea surface was 14.3°C (compared to 16.1°C at Station 2). In July <strong>2008</strong> the sea surface was<br />

20.2°C (compared to 24.0°C at Station 1 and 20.8°C at Station 2). The FTB appears to closely match<br />

the ocean temperature in the winter, with higher temperatures than the ocean in the summer months, a<br />

condition typically seen in other coastal embayments in the region.<br />

Dissolved oxygen levels measured at <strong>Bolsa</strong> <strong>Chica</strong> were within the expected range and reflected the<br />

strong influence of diurnal tidal flow, with DO levels rising and falling with tides as water masses with<br />

differing physical and biotic conditions were exchanged. Dissolved oxygen concentrations in water<br />

are determined by a number of factors including: production through photosynthesis, atmospheric gas<br />

exchange, oxygen consumption through biochemical oxygen demand and chemical oxygen demand,<br />

and saturation capacity as dictated by temperature, salinity, and barometric pressure. The condition of<br />

the FTB inlet remained suitable to provide enough tidal circulation throughout the basin to maintain<br />

DO levels generally well above 5.5 mg/L, with daily tidal peaks in the 7.5 to 8.5 mg/L range, even<br />

during the warm July month when unhealthy drops in DO can be observed in poorly circulated<br />

systems.<br />

The salinity data available reflected the absence of significant freshwater input into the FTB, with<br />

salinities similar to typical oceanic salinities.<br />

Merkel & Associates, Inc. 71

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