Barth, J. A. Oregon State University, email@example.com
Cowles, T. A. Oregon State University, firstname.lastname@example.org
Richman, J. G. Oregon State University, email@example.com
Pierce, S. D. Oregon State University, firstname.lastname@example.org
Wingard, C. Oregon State University, email@example.com
MESOSCALE PHYSICAL AND BIO-OPTICAL STRUCTURE OF THE ANTARCTIC POLAR FRONT
As part of the US SOJGOFS program, we obtained multiple, high-resolution vertical sections of physical (temperature, salinity, density, velocity) and bio-optical (fluorescence, multi-wavelength particulate absorption and attenuation) properties of the Antarctic Polar Front (APF) using SeaSoar and shipboard ADCP during cruises in austral Spring and Summer. Each cruise we conducted transects along 170W from 57S to the sea ice edge (62.3S October 1997; 67.7S January 1998) and made grid surveys at the APF.
In Spring, the N-S transect revealed sharp temperature and velocity boundaries at the APF with deep mixed layers to the north. Grid surveys of the APF captured a large meander that propagated eastward at 8 cm/s. We found evidence
for equatorward subduction of cold water from poleward of the APF. Maps along density surfaces suggest that downwelling occured upstream of the cyclonic portion of the meander and upwelling downstream. Spatially variable high fluorescence was found south of the APF, with 10-15 km wide 'tubes' of high fluorescence aligned along the front. In Summer, the N-S transect revealed a stratified surface layer with a pycnocline between 25 and 60 m across the APF region. Fluorescence was low in the APF region, but strong between 64 and 65.5S.
Day: Wednesday, Feb. 3
Time: 02:30 - 02:45pm
Location: Sweeney Center