Bottom Gravity Currents and Overflows in Deep Channels of the Atlantic Ocean 2021
DOI: 10.1007/978-3-030-83074-8_1
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Deep Water Masses of the South and North Atlantic

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Cited by 3 publications
(2 citation statements)
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“…Seismic oceanography provides a means of extending our historical record of changes in the hydrography of the deep ocean. Although the majority of seismic reflection datasets lie above continental shelves and slopes, a significant number of surveys extend into deep near-shelf regions that are key in formation of abyssal water masses (Figure 4; e.g., Dickson and Brown, 1994;Orsi et al, 1999;Morozov et al, 2021). For instance, between the years 1976 and 2011 more than 360,000 km of seismic reflection transects were acquired between the shoreline of Antarctica and regions with water depths of ≳ 5,000 m (Breitzke, 2014; note that not all of these transects are plotted in Figure 4A).…”
Section: Abyssal Water Mass Transformationsmentioning
confidence: 99%
“…Seismic oceanography provides a means of extending our historical record of changes in the hydrography of the deep ocean. Although the majority of seismic reflection datasets lie above continental shelves and slopes, a significant number of surveys extend into deep near-shelf regions that are key in formation of abyssal water masses (Figure 4; e.g., Dickson and Brown, 1994;Orsi et al, 1999;Morozov et al, 2021). For instance, between the years 1976 and 2011 more than 360,000 km of seismic reflection transects were acquired between the shoreline of Antarctica and regions with water depths of ≳ 5,000 m (Breitzke, 2014; note that not all of these transects are plotted in Figure 4A).…”
Section: Abyssal Water Mass Transformationsmentioning
confidence: 99%
“…Em seguida, a ACS é caracterizada por temperaturas no intervalo entre 0,1ºC a 2ºC, salinidade entre 34,6% a 34,7% (EMERY; MEINCKE, 1986), baixa concentração de oxigênio dissolvido e alta concentração de nutrientes (STRAMMA; ENGLAND, 1999;VIANA et al, 1998). Por último, a APAN possui temperaturas entre 1,5ºC a 4ºC, salinidade entre 34,6-35% (EMERY; MEINCKE, 1986;MOROZOV et al, 2010;SILVEIRA et al, 2000;ENGLAND, 1999), alta concentração de oxigênio dissolvido, mas é pobre em nutrientes (MOROZOV et al, 2010).…”
Section: áRea De Estudounclassified