The R/V Falkor left the Port of Corpus Christi with
near-perfect weather conditions. During
the trip to the exploration sites, the team celebrated Dr. Thomas Shirley’s 20th
birthday at sea during his 30-year career with a gourmet birthday cake and live
musical entertainment. Dr. Shirley,
Chief Scientist of the expedition, will lead the team by directing underwater multibeam
mapping, surface faunal observations, remotely operated vehicle (ROV) 3-D
videography, and geological and biological samples collected by the ROV.
Crew member Ramón sings for crew member Nona and
Dr. Shirley, who share the same birthday. Image credit: Harriet Nash
Image credit: Harriet Nash
While in transit, the science party convened to finalize the
route for multibeam data collection of all high-priority sites after a data
processing lesson from SOI’s marine technology crew. Three passes, with 10-percent overlap, will
generate data swaths that will be processed and mapped to produce detailed
3-D images of the banks. The
vessel arrived at the first site, Bad Mud Bank, at 1800. The multicolor imagery of Baker Bank, however,
generated the most excitement among scientists in the video control room on the
first day due to the site surface complexity evident immediately upon the first
pass over the site. Dr. Shirley assigned
each team member 2-hour shifts of data processing for the first 36 hours of
multibeam data collection at the South Texas Banks. By the end of day one, with only six hours of
site-specific multibeam data collection, we already completed the first of three
data swaths for the most important sites.
Dr. Wes Tunnell processes raw multibeam data.
Image credit: Harriet Nash; Schmidt Ocean Institute
Written by Harriet Nash for Harte Research Institute at Texas A&M University-Corpus Christi
Great blog! Any thoughts on why there was so much complexity seen at Baker Bank?
ReplyDeleteAdelaide: Baker Bank is an ancient drowned reef, so there still exists a lot of complexity as far as the topography and diversity.
DeleteThe spurs and grooves of the ancient drowned reef as well as continuous erosion, bioturbation, and sediment transport contribute to the rugosity of the site. Just you wait until we reveal the 3D maps of our next sites!
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