2000
DOI: 10.1007/978-94-010-0928-7_6
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Three-Dimensional Initiation of Thermohaline Fingering

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Cited by 4 publications
(2 citation statements)
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“…First of all, the global stability N 2 has to be positive. If so, the critical zone based on the local stability R ρ is 1 b R ρ b 2 (Saiki et al, 2000) for saltfingering and 1 b R ρ b 10 for diffusive convection (Kelley et al, 2003).…”
Section: Critical Thresholdsmentioning
confidence: 99%
“…First of all, the global stability N 2 has to be positive. If so, the critical zone based on the local stability R ρ is 1 b R ρ b 2 (Saiki et al, 2000) for saltfingering and 1 b R ρ b 10 for diffusive convection (Kelley et al, 2003).…”
Section: Critical Thresholdsmentioning
confidence: 99%
“…As critical thresholds are used: ρ R < 1 for thermosolutal convection, 1 < ρ R ≤ 2 for saltfingers (Saiki et al 2000), and 1 < ρ R ≥ 10 for diffusive convection (Kelley et al 2003). Necessary parameters for the cause orientated algorithm are calculated from geophysical borehole measurements of temperature-conductivity-(pressure) probes and compared to the above mentioned critical thresholds.…”
Section: Cause Orientated Interpretationmentioning
confidence: 99%