A current meter array of 3 months duration from the Newfoundland shelf
edge to the 400-m isobath gives a mean southward transport of the Lab
rador Current of 3.7 Sv with a freshwater component of 0.1 Sv. Over a
2-month period, the volume and the freshwater flow increased by 3 and
0.09 Sv, respectively. Mean currents exceeded the variable components
by a factor of 3. This estimate of the total transport of the Labrador
Current is low because the flow extends eastward of the array beyond
the 400-m isobath to at least 1000 m. The total volume transport of th
e Labrador Current through Flemish Pass is estimated roughly to range
between 6.3 and 9.8 Sv if archived current meter data are incorporated
with the observations from this array. The mean freshwater transport
is estimated to be 0.13 +/- 0.03 Sv.