Three-Dimensional Structure and Temporal Evolution of Submesoscale Thermohaline Intrusions in the North Pacific Subtropical Frontal Zone

• Published in: Journal of physical oceanography Vol. 40; no. 8; pp. 1669 - 1689
• Main Authors: SHCHERBINA, A. Y, GREGG, M. C, ALFORD, M. H, HARCOURT, R. R
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 01.08.2010
• Subjects: Earth, ocean, space; Exact sciences and technology; Experiments; External geophysics; Marine; Meteorology; Physics of the oceans; Salinity; Pacific Ocean; North Pacific; IN, North Pacific; PSW, South Atlantic, Subtropical Front; Water mass; time scales; Oceanic turbulence; Thermohaline convection; Oceanic front; subtropical zone; trajectory; intrusions; Drifting float; Mesoscale; Three dimensional structure; Three dimensional turbulence; Observation data; fresh water; meanders
• ISSN: 0022-3670; 1520-0485
• DOI: 10.1175/2010jpo4373.1

Abstract Four instances of persistent intrusive deformation of the North Pacific Subtropical Front were tagged individually by a Lagrangian float and tracked for several days. Each feature was mapped in three dimensions using repeat towed observations referenced to the float. Isohaline surface deformations in the frontal zone included sheetlike folds elongated in the alongfront direction and narrow tongues extending across the front. All deformations appeared as protrusions of relatively cold, and fresh, water across the front. No corresponding features of the opposite sign or isolated lenslike structures were observed. The sheets were O(10 m) thick, protruded about 10 km into the warm saline side of the front, and were coherent for 10–30 km along the front. Having about the same thickness and cross-frontal extent as the sheets, tongues extended less than 5 km along the front. All of the intrusions persisted as long as they were followed, several days to one week. Their structures evolved on both inertial (23 h) and subinertial (∼10 days) time scales in response to differential lateral advection. The water mass surrounding the intrusions participated in gradual anticyclonic rotation as a part of a mesoscale meander of the subtropical front. The intrusions may be interpreted as a manifestation of three-dimensional submesoscale turbulence of the frontal zone, driven by the mesoscale. Absence of large features of the opposite sign may be indicative of the asymmetry of the underlying dynamics.