Ocean current, temperature, and salinity data obtained from the wester
n Weddell Sea during the austral winter 1992 U.S.-Russian drifting ice
station experiment Ice Station Weddell 1 (ISW-1) are used to describe
water circulation and transport. Surface-to-bottom baroclinic current
s were computed by applying the geostrophic approximation to derived d
ensity data. These were corrected using current measurements obtained
from drifting current meter arrays, and the resulting total currents w
ere vertically integrated to obtain volume transports. Transport was f
ound to be northward in the region, which encompassed the western boun
dary current of the cyclonic Weddell Sea gyre. This northward transpor
t increased from south to north by more than a factor of 2, from about
12 x 10(6) m(3) s(-)1 in the southwestern Weddell to about 28 x 10(6)
m(3) s(-)1 farther north. The increase in northward transport was com
pensated for by westward flow from the interior of the gyre into the w
estern boundary region. About 5-6 x 10(6) m(3) s(-1) of the northward
transport was contained in a 300-500 m thick bottom layer of cold wate
r. This layer, whose transport increased by about 1 x 10(6) m(3) s(-1)
from south to north, was identifiable by its water mass characteristi
cs as Weddell Sea Bottom Water originating on the southwestern and wes
tern shelf regions. Its north flowing volume was consistent with past
estimates of a 1.5-2 x 10(6) m(3) s(-1) production rate coupled with a
300-400% transport increase due to entrainment during downslope flow
from the shelves to the deep basin. The maximum (northernmost) northwa
rd transport, less the bottom water transport, is consistent with prev
ious estimates for wind-driven transport in the Weddell Gyre provided
that bottom friction and the sea ice influence on wind forcing are tak
en into consideration.