Temperature and salinity variability on the eastern Newfoundland shelf: The annual harmonic
Open Access
- 1 March 1991
- journal article
- research article
- Published by Taylor & Francis in Atmosphere-Ocean
- Vol. 29 (1), 14-36
- https://doi.org/10.1080/07055900.1991.9649390
Abstract
A 36‐year time series from an oceanographic station, Sta. 27, located off St John's, Newfoundland, has been used to derive the amplitudes and phases of the annual harmonics of temperature and salinity at fixed depths from 0 to 175 m. The analysis has been also carried out for the Newfoundland and Labrador Shelf, divided into about 40 areas, using monthly mean values from the available literature. At the surface, temperature (salinity) amplitudes are about 5°C (0.5–1.0) decreasing to −4 m2 s−1 and that horizontal currents of about 0.2 m s−1 (0.1 m s−1) are representative of the upper 50 m (50–100 m). Other processes such as the annual ice cycle and runoff from the land are identified as important.Keywords
This publication has 6 references indexed in Scilit:
- The influence of Hudson Bay runoff and ice‐melt on the salinity of the inner Newfoundland ShelfAtmosphere-Ocean, 1990
- The mean barotropic circulation on the Newfoundland shelf and slopeJournal of Geophysical Research: Oceans, 1988
- The near‐surface circulation and exchange in the newfoundland grand banks regionAtmosphere-Ocean, 1985
- The Bunker Climate Atlas of the North Atlantic OceanPublished by Springer Nature ,1985
- Circulation on the newfoundland continental shelfAtmosphere-Ocean, 1983
- Oceanographic conditions at Ocean Weather ShipBravo, 1964–1974Atmosphere-Ocean, 1980