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Cold halocline in the northern California Current: An invasion of subarctic water
Author(s) -
Freeland Howard J.,
Gatien Germaine,
Huyer Adriana,
Smith Robert L.
Publication year - 2003
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2002gl016663
Subject(s) - halocline , subarctic climate , current (fluid) , oceanography , geology , downwelling , spring (device) , submarine pipeline , thermocline , salinity , upwelling , mechanical engineering , engineering
Subsurface upper ocean waters off Oregon and Vancouver Island were about 1°C cooler in July 2002 than in July 2001. The anomalously cool layer coincides with the permanent halocline which has salinities of 32.2 to 33.8, suggesting an invasion of nutrient‐rich Subarctic waters. The anomalously cool layer lies at 30–150 m. The cool anomaly is likely caused by stronger southward flow in the California Current and weaker northward flow in the Alaska and Davidson Currents during spring 2002. Other factors may include reduced coastal downwelling in late winter and early spring 2002, enhanced eastward flow in the Subarctic Current, and enhanced winter mixing offshore.