FastFind »   Lastname: doi:10.1029/ Year: Advanced Search  

Geophysical Monograph Series

 

Keywords

  • Hydrothermal vents—Congresses
  • Hydrothermal deposits—Congresses
  • Hydrothermal vent ecology—Congresses

Index Terms

  • 4599 Oceanography: Physical: General or miscellaneous
  • 8135 Tectonophysics: Hydrothermal systems
  • 4520 Oceanography: Physical: Eddies and mesoscale processes
  • 4532 Oceanography: Physical: General circulation

Article

GEOPHYSICAL MONOGRAPH SERIES, VOL. 91, PP. 347-356, 1995

Oceanic hydrothermal circulation: Mesoscale and basin-scale flow

K. R. Helfrich and K. G. Speer

An understanding of the circulation, both ambient and forced, in the vicinity of hydrothermal sources is important not only for physical oceanographic problems, but also for other disciplines. For scientists interested in heat flux from a ridge crest segment the direct measurement of heat flux from hydrothermal sources is not yet feasible. Identification of all the continuous hydrothermal sources is difficult at best, let alone the measurement of each one. Furthermore, episodic tectonic and volcanic activity has been shown to result in massive hydrothermal releases know as megaplumes [Baker et al., 1989; Chadwick et al., 1991]. Although observation of such events is a goal of the RIDGE program it is a task that requires both quick response and luck. However, for both continuous and event sources, estimates of heat flux can be attempted from observations of the water column, which acts as an integrator. The key to this estimation is the availability of observations of sufficient resolution and duration for an adequate budget to be constructed and the availability of suitable models of the flow caused by hydrothermal discharge. The most familiar model of this type is the buoyant plume model of Morton et al. [1956] which has been used numerous times to relate observed plume characteristics such as rise height or centerline temperature to source heat flux [e.g., Little et al., 1987].

Citation: Helfrich, K. R., and K. G. Speer (1995), Oceanic hydrothermal circulation: Mesoscale and basin-scale flow, in Seafloor Hydrothermal Systems: Physical, Chemical, Biological, and Geological Interactions, Geophys. Monogr. Ser., vol. 91, edited by S. E. Humphris et al., pp. 347–356, AGU, Washington, D. C., doi:10.1029/GM091p0347.

Cited By

Please wait one moment ...