Temperature, Salinity and Density Along the Standard Bonavista Transect
The trough between the northern Grand Bank and the Funk Island Bank has recently been identified as a likely corridor along which a significant biomass of northern cod migrate to the inshore areas along the east coast of Newfoundland during late spring and early summer. This report provides synoptic, monthly average, and annual time series of temperature, salinity, and density for the NAFO Cape Bonavista standard transect based on all data available from 1930-92 and gives a review of the spatial and temporal distribution of the data. A brief descriptive analysis of various indices describing the temperature and salinity field along the transect is presented, including a discussion of the 1948-92 time series of the cross-sectional area of the Cold Intermediate Layer. Summer temperature and salinity anomalies (referenced to a July-August average for 1948-92) are presented for 1984-92.
"The trough between the northern Grand Bank and the Funk Island Bank has recently been identified as a likely corridor along which a significant biomass of northern cod migrate to the inshore areas along the east coast of Newfoundland during late spring and early summer. This report provides synoptic, monthly average, and annual time series of temperature, salinity, and density for the NAFO Cape Bonavista standard transect based on all data available from 1930-92 and gives a review of the spatial and temporal distribution of the data. A brief descriptive analysis of various indices describing the temperature and salinity field along the transect is presented, including a discussion of the 1948-92 time series of the cross-sectional area of the Cold Intermediate Layer. Summer temperature and salinity anomalies (referenced to a July-August average for 1948-92) are presented for 1984-92."@en
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Mer Température Terre-Neuve Bonavista, Région du cap.
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