1988
DOI: 10.1080/07055900.1988.9649304
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Sea surface temperature variability in the shelf‐slope region of the Northwest Atlantic

Abstract: Sea surface temperature (SST) variability in the shelf-slope region of the northwest Atlantic is described and then explained in terms of latent and sensible heat exchange with the atmosphere. The basic data are primarily engine-intake temperature measurements made by merchant ships over the period

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Cited by 40 publications
(51 citation statements)
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“…S11). These scales are comparable to those of climate forcing in the NWA and NEA (22)(23)(24)(29)(30)(31). Thus, these analyses reveal that, contrary to the prevailing assumption (2,16,17), the scales of fishing mortality are equivalent to those of atmosphere-ocean forcing, and could account for a significant portion of the large-scale synchrony that prevails in these cod stocks.…”
Section: Significancementioning
confidence: 76%
See 1 more Smart Citation
“…S11). These scales are comparable to those of climate forcing in the NWA and NEA (22)(23)(24)(29)(30)(31). Thus, these analyses reveal that, contrary to the prevailing assumption (2,16,17), the scales of fishing mortality are equivalent to those of atmosphere-ocean forcing, and could account for a significant portion of the large-scale synchrony that prevails in these cod stocks.…”
Section: Significancementioning
confidence: 76%
“…In sharp contrast to the unimodal distribution of the fishing mortality to which these NWA cod stocks were subjected, and to its corresponding effect on SSB, NWA sea surface (22) and bottom (23) temperatures were characterized by a strong bimodal spatial distribution, the boundary separating positive and negative temperature anomalies being located on the northeast Scotian Shelf (stock 4) (Fig. 1A).…”
Section: Significancementioning
confidence: 97%
“…Significant efforts have been made in the past to determine the general circulation, hydrographic distributions and associated seasonal variability of the ECS (Smith and Schwing, 1991;Lynch et al, 1996;Sheng and Thompson, 1996;Colbourne et al, 1997;Loder et al, 1998;Xue et al, 2000;Sheng et al, 2001;Han and Loder, 2003;Han et al, 2008). Efforts have also been made to examine the interannual variability over this region (Thompson et al, 1988; Petrie et al, 1992;Petrie and Drinkwater, 1993;Han and Tang, 2001;Han, 2007). Many questions, however, remain unanswered regarding the general circulation and associated temporal and spatial variability over the region.…”
Section: Introductionmentioning
confidence: 99%
“…1a). Previous studies have demonstrated that the ECS is the most variable area of the North Atlantic and Pacific oceans (Thompson et al, 1988), with the largest seasonal variations in water temperature, about 16°C, occurring over the Scotian Shelf and the Middle Atlantic Bight. Significant efforts have been made in the past to determine the general circulation, hydrographic distributions and associated seasonal variability of the ECS (Smith and Schwing, 1991;Lynch et al, 1996;Sheng and Thompson, 1996;Colbourne et al, 1997;Loder et al, 1998;Xue et al, 2000;Sheng et al, 2001;Han and Loder, 2003;Han et al, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…The sea surface temperature (SST) over the study region has a strong seasonal cycle, with a mean range of about 16°C (Thompson, Loucks and Trites, 1988), largely due to the intense negative and positive heat fluxes at the sea surface from the atmosphere to the ocean in winter and summer respectively. The interannual and decadal variability of temperature and salinity on the SS is affected significantly by variations of the westward transport of the Labrador Current through the shelf-slope exchange (Petrie and Drinkwater, 1993).…”
Section: Introductionmentioning
confidence: 99%