13.07.2015 Views

Vibrio in seafood - FAO.org

Vibrio in seafood - FAO.org

Vibrio in seafood - FAO.org

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

The predicted mean log V. parahaemolyticus level versus temperature for the temperature-onlyregression is shown <strong>in</strong> Figure 2.7. Clearly, this relationship is comparable with that which would beobta<strong>in</strong>ed by fix<strong>in</strong>g the sal<strong>in</strong>ity to a near optimal value (22 ppt) <strong>in</strong> the prediction equation based on bothwater temperature and sal<strong>in</strong>ity. The temperature-only regression was used to model the relationshipbetween temperature and density of total V. parahaemolyticus at time of harvest.4.53.52.51.50.50 5 10 15 20 25 30 35Water temperature (º C)limit ofdetectionFigure 2.7: Observed log 10 V. parahaemolyticus (Vp) numbers <strong>in</strong> oysters versus water temperature atdifferent sal<strong>in</strong>ities (20 ppt (○)) <strong>in</strong> comparison to predicted log 10numbers (solid l<strong>in</strong>e) and 95% confidence limits (dashed l<strong>in</strong>es) based on temperature only regressionmodel.2.2.5.3.2 Water Temperature DistributionsIn the United States FDA-VPRA (Anonymous, 2001), regional and seasonal distributions of watertemperatures were developed based on accumulated records from coastal water buoys (National Buoy DataCenter data). Seasons were def<strong>in</strong>ed by calendar month: w<strong>in</strong>ter (January-March), spr<strong>in</strong>g (April-June),summer (July-September) and fall (October-December). For each region and season a shallow water buoywas selected as represent<strong>in</strong>g the water temperature distribution for oyster harvest areas with<strong>in</strong> thatregion/season comb<strong>in</strong>ation. The available database for most buoys has hourly water temperatures from1984 up to the present time, with occasional data gaps due to <strong>in</strong>strumentation malfunction. The correlationbetween water temperature and the ambient air temperature that oysters are subject to after they areharvested was accounted for by select<strong>in</strong>g buoys for which air temperature records were also available.Because oyster harvest<strong>in</strong>g <strong>in</strong> the United States outside of the Pacific Coast region commencesearly <strong>in</strong> the morn<strong>in</strong>g and ends mid or late afternoon, the daily water temperature recorded at noon wasconsidered to represent an average daily temperature. The distribution of these "average" temperatureswith<strong>in</strong> a given region and season varies from year-to-year with wider variations occurr<strong>in</strong>g dur<strong>in</strong>g thetransitional seasons of spr<strong>in</strong>g and fall.With<strong>in</strong> a given year, the distribution of the noon water temperature was found to be unimodalwith<strong>in</strong> a given range. This empirical distribution is adequately approximated as a normal distributionprovided that no weight is given to implausible values outside the historical range of values that may be21

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!