Hydrographic Variability in the Waters of the Gulf of St. Lawrence, the Scotian Shelf and the Eastern Gulf of Maine

This paper examines the hydrographic variability within the Gulf of St. Lawrence, the Scotian Shelf and the eastern Gulf of Maine, including the Bay of Fundy, during the decade 1991–2000. Comparisons are made with previous decadal means to place the 1990s into a longer-term perspec-tive. The 1990s d...

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Bibliographic Details
Main Authors: Nafo Subarea During, Kenneth F. Drinkwater, Denis Gilbert
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
decadal variability
oceanography
salinity
stratification
temperature
Newfoundland
Tive
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.510.746
http://journal.nafo.int/34/drinkwater2/6-drinkwater.pdf
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Summary:This paper examines the hydrographic variability within the Gulf of St. Lawrence, the Scotian Shelf and the eastern Gulf of Maine, including the Bay of Fundy, during the decade 1991–2000. Comparisons are made with previous decadal means to place the 1990s into a longer-term perspec-tive. The 1990s decadal means of the near-surface salinity were the lowest ever recorded for the northern Gulf of St. Lawrence, the Scotian Shelf and the Bay of Fundy. These low salinities were advected into these regions from the Labrador and Newfoundland Shelves and led to record or near record high vertical stratification in the upper layers of the water column. Also during the 1990s, the decadal means of the temperature of the intermediate layer waters (approximately 30–150 m) were well below normal throughout the Gulf of St. Lawrence and over much of the Scotian Shelf. Similar low temperatures were first observed in the late 1980s and were mainly caused by advection from the Labrador and Newfoundland Shelves, although local atmospheric cooling also contributed. In the deep channels and basins of NAFO Subarea 4, near-bottom decadal mean temperatures were high and linked to the persistence of Warm Slope Water along the shelf break. A notable exception occurred in 1998 when Labrador Slope Water moved southward along the continental slope as far as the Mid-dle Atlantic Bight, pushing the Warm Slope Water offshore. This much colder water subsequently penetrated onto the Scotian Shelf and into the Gulf of Maine resulting in the coldest conditions in the deep basins since the 1960s.

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