2023
DOI: 10.1007/978-3-031-16575-7_49
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The Black Sea Deep-Water Circulation: Recent Findings and Prospects for Research

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Cited by 1 publication
(2 citation statements)
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“…To calculate the effects of mixing OM remineralization products into this environment, we use a volume of 32,398 km 3 , which is equivalent to ∼43% of the total volume of the abyssal benthic boundary layer (75,137 km 3 ). This reduced effective volume is an attempt to account for incomplete lateral mixing at depth and can be refined by future studies of advective flow dynamics within the layer (Markova, 2023). The amount of OM respired "instantaneously" in situ was varied from 0 to 40 Tmol C, which is equivalent to 0-1.76 Pg (Gt) CO 2 .…”
Section: The Black Sea: Biogeochemical Impacts Of Organic Matter Sequ...mentioning
confidence: 99%
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“…To calculate the effects of mixing OM remineralization products into this environment, we use a volume of 32,398 km 3 , which is equivalent to ∼43% of the total volume of the abyssal benthic boundary layer (75,137 km 3 ). This reduced effective volume is an attempt to account for incomplete lateral mixing at depth and can be refined by future studies of advective flow dynamics within the layer (Markova, 2023). The amount of OM respired "instantaneously" in situ was varied from 0 to 40 Tmol C, which is equivalent to 0-1.76 Pg (Gt) CO 2 .…”
Section: The Black Sea: Biogeochemical Impacts Of Organic Matter Sequ...mentioning
confidence: 99%
“…The abyssal Black Sea is characterized by a relatively well‐mixed benthic boundary layer below ∼1,750 m water depth (Murray et al., 1991). Water movement and density homogenization within the deep boundary layer are driven by thermal convection (Ivanov & Samodurov, 2001), while mixing within the mid‐water column is driven primarily by mesoscale cyclonic and occasional anticyclonic eddies (Markova, 2023). Currents in the deep Black Sea thus differ from the well‐known rim current system in surface water.…”
Section: Introductionmentioning
confidence: 99%