Abstract

Previous work has shown that sooty shearwater (Puffinus griseus) harvest data are able to predict shifts in the Southern Oscillation Index (SOI) by approximately 4–14 months. In this study, the mechanisms of this relationship are examined. The oceanographic regions in our study area that best explain variation in SOI from 1 to 12 months after peak shearwater chick size were Southeast of New Zealand along the Polar and sub-Antarctic fronts and in the southern regions of the sub-Antarctic water zone. Spearman correlations of oceanographic parameters show that within the sub-Antarctic water and core foraging areas of sooty shearwaters, positive significant relationships exist between SOI and wind speed, significant wave height charnock parameter, and chick size. A model that combined the significant parameters from both offshore regions and the nearshore foraging area of sooty shearwaters, had a Pearson’s correlation of r > 0.8 for SOI values from 0 to 14 months after peak chick size. A combination of parameters and regions best explain the variation in the SOI data, however the most important variables are those that represent general turbulence in the sub-Antarctic water and Polar front regions (i.e., wind speed, and significant wave height). Using seabirds as an indicator of upcoming climate events could lead modelers to regions of importance for the formation of El Nino events, and highlights the importance of integrating ecological signals into climate models.

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