The Mixing Zephyr Pages

CTDT Groundtruth Opportunities

Overall Coverage of the Mixing Zephyr Night and Alvin Programs

This first map shows the traces of the all Mixing Zephyr (MZ) CTDT casts in blue, overlain by all of the MZ Alvin dive tracks in yellow. Along each CTDT trace, the locations where the CTDT instruments were within 50 meters of the local sea floor are highlighted in red.

Notice that because the ALVIN submersible usually descends and ascends directly upon a dive target -- historically (during the MZ cruises?) a particular vent field (initially located via CTDT surveys) -- very few ALVIN tracks transgress the perimeters of the known vent fields. This means that few observations of what the sea floor is like between known fields were obtained via Mixing Zephyrs dive program.

Diffuse Flow Sites: Cirque and Dune

Alvin Dive 2931 is an exceptional dive in that one of its targets -- located based on near-bottom CTDT measurments -- was hypothesized to be associated with diffuse flow, rather than a focussed source of hydrothermal effluent. Impressively, near the target divers encountered two areas of diffuse flow venting through tube worm beds atop N-S basaltic pillow ridges, located about 1 km west of the Salty Dawg vent field.

In retrospect, the sea floor observation of diffuse flow at a location specified on the basis of CTDT information is rather remarkable, and certainly unprecedented. Since the cost of locating and mapping potentially-extensive areas via submersible is discouraging, it is worth re-examining the Mixing Zephyr CTDT casts that traversed near where the diffuse flow was observed. In turn, the ALVIN dive 2931 observations of diffuse flow separated from known fields of hydrothermal activity represent one of the best opportunities in all of the MZ data to "groundtruth" the CTDT measurements. This map shows dive 2931 proceeding generally from south to north. The first dive target -- the location of suspected diffuse flow -- is indicated by a magenta dot, while the locations of the 2 observed areas of diffuse flow are indicated by magenta stars. One area has been named "Cirque" and the other "Dune."

Name	X	Y	Longitude		Latitude 		Depth	Water Samples
Cirque?	5878    9562	129.085912765213	47.9799124134209	2131	GT Yellow; M Yellow;
Dune?	5882    9738	129.085859274975	47.9814955743456	2127	GT Purple; M Red;

What exactly is the evidence of diffuse effluent in the CTDT data? How does the signature of diffuse flow differ from the CTDT signals caused by focussed hydrothermal flow, or can they not be differentiated without further (chemical) information? Where else in the MZ CTDT observations are similar near-bottom signatures observed? Or is all of the water near the seafloor (or in the Cirque-Dune depth range) marked by similar T,S,Z characterisics?


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The Mixing Zephyr Pages
Maintained by Russ McDuff (mcduff@ocean.washington.edu)
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Content Last Modified 7/17/97 SRV
Page Last Built 7/17/97