title: Evidence for Oceanic Frontogenesis off Oregon.
abstract: Bathythermograms recorded off Newport, Oregon, show marked positive gradients during the period of cessation of summer upwelling. It is suggested that these are related to the formation of a shear zone or "front" between oceanic water and shelf water that has been exposed to the surface and modified.
authors.forename: J G
authors.initials: JG
authors.lastname: Pattullo
authors.forename: W B
authors.initials: WB
authors.lastname: McAlister