WebJul 12, 2024 · the Chiniak trough (Fig. 5). On this pro le, we iden-tify a single high-angle splay fault near CDP 685, which lies along strike of the tsunamigenic fault . identi ed on … WebPollock biomass estimates for August 2001 in Barnabas and Chiniak Troughs. Significant differences among either the juvenile or adult pollock biomass estimates in response to …
Effect of ocean conditions on the cross‐shelf distribution of …
WebTrough is 110 m deep. Chiniak Trough, sepa rating North and Middle Albatross banks, has an apparent sill depth of 145 m. Kiliuda Trough, southernmost of the three cuts, lies … WebThe presence of mesoscale eddies in the gulf had no unique influence on currents or salinity in the troughs. Tidal mixing was strongest in Chiniak Trough, and this introduced cold, nutrient-rich ... pho-bowl
Effect of ocean conditions on the cross‐shelf distribution …
WebIn Chiniak Trough, capelin were most abundant along steep topographic gradients at the edges of the trough and in a deep region near Cape Chiniak, whereas the capelin–age-0 mix (2000) or capelin (2001) concentrations were observed in slope water intrusions over the outer shelf in Barnabas Trough. Results suggest that habitat selection of ... WebTrough is 110 m deep. Chiniak Trough, sepa rating North and Middle Albatross banks, has an apparent sill depth of 145 m. Kiliuda Trough, southernmost of the three cuts, lies between Middle and South Albatross banks and has a sill depth of 150 m. Amatuli Trough, the most north erly feature in the study area, lies north of Port WebIn Chiniak Trough, capelin were most abundant along steep topographic gradients at the edges of the trough and in a deep region near Cape Chiniak, whereas the capelin–age‐0 mix (2000) or capelin (2001) concentrations were observed in slope water intrusions over the outer shelf in Barnabas Trough. Results suggest that habitat selection of ... pho boulder