The North Atlantic east of the Grand Banks presents a thermal front from 40
degrees to 50 degreesN between the warm North Atlantic Current (NAC) and t
he cold Labrador Current. Here we use the trajectories of 84 isopycnal RAFO
S floats deployed on the 27.2 and 27.5 sigma (T) surface in 1993-1995 and 2
18 surface drifters deployed by the International Ice Patrol and the Instit
ut fur Meereskunde (Kiel, Germany) between 1978 and 1993 to understand the
pathways of the NAG. The mean flow pattern, kinetic energy, directional sta
bility, and most probable path through 1 degrees by 1 degrees boxes are der
ived for each of the three surfaces. Speed and kinetic energy decrease with
depth, although directional stability is comparable at all levels. The axi
s of the NAG, which follows the 4000 m isobath along the western boundary,
is described by mean kinetic energy (MKE) Values surpassing 100 cm(2) s(-2)
on the float surfaces and correspond to regions with directional stabiliti
es in excess of 60%. Maximum values of eddy kinetic energy are found just o
ffshore of the maximum MKE associated with the NAC main pathway and decreas
e rapidly to the east. Two cyclonic meanders are identified at 44 degreesN,
45 degreesW near the Newfoundland Seamounts and at 46 degreesN, 42 degrees
W near Flemish Cap. The main difference between the patterns derived for th
e surface drifters and floats was the greater eastward extent of the cyclon
ic trough st 44 degreesN and intensity of the Mann Eddy (42 degreesN, 44 de
greesW) during the float sampling period (1993-1995).