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| Multibeam Data - Volcano |
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Question: What is the difference between topographic and bathymetric maps? Why are these kinds of maps useful? |
Data is collected almost constantly. The multi-beam is not on when the ship is stopped unless the drift is more than 1 knot. Additionally, the multi-beam is not run when the ship is passing through very heavy ice. If there are leads, then the multi-beam will be left on. Leads are patches of open water between the ice. All the data must then be edited and compiled. Usually there are people on board ship who help with the editing although some of the time, Kathleen does part of it herself. Data that is gathered on the cruise is given to the chief scientist. At times there may be 20-30 gigabytes of data.
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Question: How big is a gigabyte in relation to a megabyte? |
On this cruise, one of Kathleen’s duties included mapping an underwater volcano. Take a look at the map to find out a little of what’s happening below the sea surface.
Parting Thoughts: Kathleen loves her job and has no plans to leave. If you’re considering a similar career, her job is not available.

This special report was made possible by the NSF Office of Polar Programs, Antarctic Sciences Section, Award Nos. ANT04-44134 University of California-San Diego Scripps Institution of Oceanography (B. Gregory Mitchell, Farooq Azam, Katherine Barbeau, Sarah T. Gille, Osmund Holm-Hansen); ANT04-43403 University of Hawaii (Christopher I. Measures, Karen E. Selph); ANT04-44040 University of Massachusetts Boston (Meng Zhou); ANT04-43869 Woods Hole Oceanographic Institution (Matthew A. Charette), for the study entitled "Collaborative Research: Plankton Community Structure and Iron Distribution in the Southern Drake Passage".