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Near-field variability of the TAG non-buoyant plume, 26°N, Mid-Atlantic Ridge
EPSL ELSEVIER
Earth and Planetary Science Letters 128 (1994) 701
Erratum
Near-field variability of the TAG non-buoyant plume, 26°N, Mid-Atlantic Ridge E a r t h P l a n e t . Sci. L e t t . 127 ( 1 9 9 4 ) 1 - 1 0
M.D. Rudnicki, R.H. James, H. Elderfield Department of Earth Sciences, Cambridge Uniuersity, Downing Street, Cambridge CB2 3EQ, UK
The publisher apologizes for the switching of figure captions 1-3 in this paper. The figure order itself is correct as placed in the article; the correct order of captions follows below. Fig. 1. Contoured sections of (a) nephels, (b) potential temperature and (c) salinity, from a time series CTD study of the TAG non-buoyant plume. The x-axis represents the nine hour duration of the study, and the depth of the instrument is shown by the white trace. Start time 495-21:42:20, end time 496-06:48:03, station CD77414. Fig. 2. Representative CTD sections of the TAG non-buoyant plume. Thick line = particle concentration (uncalibrated volts); thin line = potential temperature (°C), light zig-zag line = salinity (p.s.u.). (a) Downcast 1. (b) Upcast 2. (c) Downcast 6. (d) Upcast 10. Fig. 3. Plot of the particle plume together with o-0 isopycnals. The calculated model height of neutral buoyancy of an 80 MW plume is also shown (dashed line).
Elsevier Science B.V.
SSDI 0 0 1 2 - 8 2 1 X ( 9 4 ) 0 0 2 2 5 - 8
Earth and Planetary Science Letters 128 (1994) 701
Erratum
Near-field variability of the TAG non-buoyant plume, 26°N, Mid-Atlantic Ridge E a r t h P l a n e t . Sci. L e t t . 127 ( 1 9 9 4 ) 1 - 1 0
M.D. Rudnicki, R.H. James, H. Elderfield Department of Earth Sciences, Cambridge Uniuersity, Downing Street, Cambridge CB2 3EQ, UK
The publisher apologizes for the switching of figure captions 1-3 in this paper. The figure order itself is correct as placed in the article; the correct order of captions follows below. Fig. 1. Contoured sections of (a) nephels, (b) potential temperature and (c) salinity, from a time series CTD study of the TAG non-buoyant plume. The x-axis represents the nine hour duration of the study, and the depth of the instrument is shown by the white trace. Start time 495-21:42:20, end time 496-06:48:03, station CD77414. Fig. 2. Representative CTD sections of the TAG non-buoyant plume. Thick line = particle concentration (uncalibrated volts); thin line = potential temperature (°C), light zig-zag line = salinity (p.s.u.). (a) Downcast 1. (b) Upcast 2. (c) Downcast 6. (d) Upcast 10. Fig. 3. Plot of the particle plume together with o-0 isopycnals. The calculated model height of neutral buoyancy of an 80 MW plume is also shown (dashed line).
Elsevier Science B.V.
SSDI 0 0 1 2 - 8 2 1 X ( 9 4 ) 0 0 2 2 5 - 8