TY - JOUR
T1 - Features of physical oceanography in the oceans near the Prydz Bay during the 1998/1999 austral summer
AU - Pu, Shuzhen
AU - Hu, Xiaomin
AU - Dong, Zhaoqian
AU - Xiang, Baoqiang
AU - Yu, Weidong
PY - 2006
Y1 - 2006
N2 - Thermohaline features, spatial extensions, and depths of the antarctic circumpolar deep water, the antarctic bottom water, and the upper layer water near the Prydz Bay (including the Prydz Bay summer surface water, the antarctic winter water, and the Prydz Bay shelf water) are analyzed and studied by use of the full depth CTD data obtained in the Southern Ocean near the Prydz Bay during the 1998/1999 austral summer. The northward extension of the shelf water, the thickness of the temperature inversion layer, the minima in the vertical temperature profile and the vertical temperature gradient are interpreted. On the basis of analysis of gravitational potential field, the geostrophic current and the geostrophic volume transport are calculated to determine the location of the strongest current in the zonal circulation near the Prydz Bay and to find the spatial variability of the volume transport in the 64° -66.5°S zone. In addition, the central location, the frontal strength, the vertical depth and thickness of the continental water boundary (CWB) are estimated from the CTD data to expound the spatial variability of CWB in the study area (64°-66.5°S, 70°-75° E).
AB - Thermohaline features, spatial extensions, and depths of the antarctic circumpolar deep water, the antarctic bottom water, and the upper layer water near the Prydz Bay (including the Prydz Bay summer surface water, the antarctic winter water, and the Prydz Bay shelf water) are analyzed and studied by use of the full depth CTD data obtained in the Southern Ocean near the Prydz Bay during the 1998/1999 austral summer. The northward extension of the shelf water, the thickness of the temperature inversion layer, the minima in the vertical temperature profile and the vertical temperature gradient are interpreted. On the basis of analysis of gravitational potential field, the geostrophic current and the geostrophic volume transport are calculated to determine the location of the strongest current in the zonal circulation near the Prydz Bay and to find the spatial variability of the volume transport in the 64° -66.5°S zone. In addition, the central location, the frontal strength, the vertical depth and thickness of the continental water boundary (CWB) are estimated from the CTD data to expound the spatial variability of CWB in the study area (64°-66.5°S, 70°-75° E).
KW - Circulation
KW - Front
KW - Prydz Bay
KW - Southern Ocean
KW - Water masses
UR - https://www.scopus.com/pages/publications/33847383700
M3 - Article
AN - SCOPUS:33847383700
SN - 0253-505X
VL - 25
SP - 1
EP - 14
JO - Acta Oceanologica Sinica
JF - Acta Oceanologica Sinica
IS - 6
ER -