8/8/96
Cruise Plan for R/V Melville - 3/26/97-4/26/97
Project: U.S.-Australia Cooperative Study of the Northern Branch of the
Antarctic Circumpolar Current
Chief Scientist, Doug Luther, Univ. of Hawaii
Co-P.I.'s
Jim Richman, OSU
Randy Watts, URI
Alan Chave, WHOI
Jean Filloux, SIO
Science Party - Not determined at this time.
The principal task of this cruise is to recover 9 full-depth current-meter
moorings, and 40 small self-contained seafloor instruments deployed in
March-April, 1995, in an elongated array extending from approximately 47S to
54.5S, 141E to 145E, SSW of Tasmania. The array spans the northern (strongest)
current jet associated with the Antarctic Circumpolar Current (ACC). The
experiment was designed to evaluate the important momentum and energy balances
in the ACC. The experiment also has goals relating to the intensity and
dynamics of the total transport of water and heat through the array, which are
relevant to WOCE objectives.
All the deployed instrumentation will be recalled acoustically. The
horizontal electrometers (18), bottom pressure recorders (4), and inverted echo
sounders (18) all are very small packages (usually a single 17" glass sphere in
a plastic hard hat), requiring reasonably good weather for radio and visual
detection when at the surface, and requiring precision ship maneuvering for
pickup.
Depending on the availability of a CTD from our Australian collaborators,
we will collect full-depth CTD profiles over at least the 18 inverted echo
sounders before they are recovered. Time permitting, we will also attempt to
complete a high-resolution CTD section from 54.5S to Tasmania (approximately 25
full-depth CTD profiles), all the while collecting direct measurements of
near-surface currents with the ship's 150 kHz ADCP, using the Ashtech 3DF GPS
receiver for position and heading. The focus of this CTD/ADCP section is to
provide additional information on the strength of the westward currents just
north of our array relative to the eastward currents that exist in the ACC.
Dr. Antony White of Flinders University of South Australia deployed 4
magnetometers within our electrometer array in April, 1996, and has requested
time on this cruise to recover those instruments. White's request will be
accommodated on a time permitting basis. [While the sub-diurnal electric fields
are oceanically induced, the super-diurnal fields are dominated by
ionospherically generated EM waves and can be combined with the magnetometer
data to provide information on the conductivity of the crust and upper mantle.]