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Crone, Timothy J. - Lamont-Doherty Earth Observatory, Columbia University
Tidally-Forced Flow Variability Within Mid-Ocean Ridge Hydrothermal Systems: Models and Measurement Techniques
0 1 2 3 4 5 6 0 0.2 0.4 Velocity (km/s) Poisson's Ratio
0 1 2 3 4 5 6 0 0.2 0.4 Velocity (km/s) Poisson's Ratio
o f O c e a n o s i t y o f W a s h
A large body of evidence indicates that fluid flow rates within mid-ocean ridge hydrothermal systems may be highly variable [e.g. Baker, 1994; Fornari et al., 1998; Lilley et al., 2003]. And recent studies show that flow within these systems may be strong
Modeling the effects of tidal loading on mid-ocean ridge hydrothermal systems
Experiments in Fluids manuscript No. (will be inserted by the editor)
The Sound Generated by Mid-Ocean Ridge Black Smoker Hydrothermal Vents
Figure 1. Photograph of the digital acoustic recording system deployed at the Sully vent in September of 2004. We
