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Final Technical Report: - Southwest Fisheries Science Center - NOAA

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4.6.2 Seasonal Predictive Ability<br />

Results indicated that inter-annual variability in environmental parameters can<br />

explain part of the variation in the seasonal distribution patterns of some cetacean<br />

species, particularly for species with large numbers of sightings during the summer<br />

survey periods (Becker 2007). Seasonal geographic patterns in ranked species density<br />

were captured for three of the five species considered. Density plots for Dall’s porpoise<br />

(Fig. 24) illustrate a species for which summer models were effective at predicting the<br />

southward shift of animals during winter. However, the predictions for northern right<br />

whale dolphins demonstrate that extreme over-predictions can result in the areas off<br />

northern California where waters were cooler during winter than observed during the<br />

summer surveys (dark blue shading in Fig. 24B). Additional surveys are required to fully<br />

characterize environmental variability and improve predictive performance sufficiently to<br />

apply these models quantitatively. In particular, model input data must include the full<br />

range of conditions for the temporal/spatial period they are predicting, i.e. cold-water<br />

conditions during winter. If possible, future seasonal model development and evaluation<br />

should also include a broader range of cold-season oceanographic conditions to<br />

characterize inter-annual variation. A final complication is that some cetaceans found in<br />

the CCE during the warm season are migratory and nearly absent in the cold season. For<br />

these reasons, we did not make any predictions of cetacean densities in one season from<br />

data that were collected in another.<br />

4.7 Model Validation<br />

Data from the novel 2005 (CCE) and 2006 (ETP) SWFSC cetacean surveys were<br />

used to validate the final encounter rate and group size models constructed using data<br />

from 1991-2001 for the CCE and from 1986-2003 for the ETP. To assess the models’ fit<br />

to the validation data set and to examine the inter-annual variability in model predictions,<br />

density was predicted separately for each survey year. Methods used to evaluate model<br />

fit included visual inspection of geographic contour plots of the annual density<br />

predictions and computation of geographically stratified ratios of observed to predicted<br />

density.<br />

4.7.1 California Current Ecosystem Models<br />

When the CCE models built using 1991-2001 survey data were used to predict<br />

density across all survey years (1991-2005), density ratios (density calculated using<br />

standard line-transect methods divided by density predicted by the habitat model) ranged<br />

from 0.62 (Baird’s beaked whale) to 1.44 (northern right whale dolphin) (Table 18).<br />

Density ratios for the novel year (2005) predictions were more variable, ranging from<br />

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