2010
DOI: 10.1016/j.jmarsys.2009.07.008
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Identification, characteristics and seasonal evolution of surface thermal fronts in the Argentinean Continental Shelf

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Cited by 77 publications
(60 citation statements)
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“…In addition, there are smaller local frontal systems in deeper bays and gulfs along the arid Patagonian coastline. These front systems result from isolated waters that are formed by interplay of high evaporation during summer, the shelf current systems and riverine inputs (Acha et al, 2004;Rivas and Pisoni, 2010). Current circulation suggests that tides, wind and bottom topography, for instance the ridge at the mouth of the San Jorge Gulf (SJG), are the main local forcing mechanisms in the Patagonian gulfs (Tonini et al, 2006;Palma et al, 2008;Matano et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…In addition, there are smaller local frontal systems in deeper bays and gulfs along the arid Patagonian coastline. These front systems result from isolated waters that are formed by interplay of high evaporation during summer, the shelf current systems and riverine inputs (Acha et al, 2004;Rivas and Pisoni, 2010). Current circulation suggests that tides, wind and bottom topography, for instance the ridge at the mouth of the San Jorge Gulf (SJG), are the main local forcing mechanisms in the Patagonian gulfs (Tonini et al, 2006;Palma et al, 2008;Matano et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…Marrari et al [3] reported that the availability of adequate food (high presence of phytoplankton and zooplankton), suitable thermal and salinity ranges, the presence of marine fronts [1,4], and the oceanic circulation that favors a retention mechanism, produce an appropriate environment for successful larval fish development. Therefore, the physical and biological characteristics of the El Rincón area generate a rich habitat of valuable commercial species, which are very important for the local artisanal fisheries [5].…”
Section: Introductionmentioning
confidence: 99%
“…The existence of a salinity and a thermal front in the study area are generated by bathymetry changes and dilution effects, combined with the northern advection of San Matí as Gulf waters, particularly in winter [2,4] (Figure 1c). These waters are characterized by high salinity values due to the dominance of evaporation over the precipitation in the water balance of the Gulf [2].…”
Section: Introductionmentioning
confidence: 99%
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“…This is widely used to define the physical environment, and impacts the variability of marine ecosystems [1,2], and is designated an Essential Climate Variable. Water masses defined by marine thermal fronts are often denoted by using SST gradient fields as a proxy, thus identifying regions of optimal conditions for growth of marine phytoplankton (nutrients, light, mixing, and upwelling) and, in many cases, enhanced trophic levels of productivity [3][4][5][6][7]. The spatial and temporal patterns in SST fields are a key characteristic of fisheries ecosystems, having implications for sustainable management [8,9].…”
Section: Introductionmentioning
confidence: 99%