The sources of the Agulhas Current are the East Madagascar
Current, the Mozambique Current and a recirculated part of the south-west
Indian subgyre (a smaller circular current within a gyre)south of Madagascar.
The flow of the Agulhas Current is directed by the topography. The current
follows the continental shelf from Maputo to the tip of the Agulhas Bank (250
km south of Cape Agulhas). Here the momentum of the current overcomes the
vorticity balance holding the current to the topography and the current leaves
the shelf.
The core of the current is defined as where the surface
velocities reaches 100 cm/s (39 in/s), which gives the core an average width of
34 km (21 mi). The mean peak speed is 136 cm/s (54 in/s), but the current can
reach 245 cm/s (96 in/s.
As the Agulhas Current flows south along the African east
coast, it tends to bulge inshore frequently, a deviation from the current's
normal path known as Agulhas Current meanders (ACM). These bulges are
occasionally (1-7 times per year) followed by a much larger offshore bulge,
known as Natal pulses (NP). Natal pulses move along the coast at 20 km (12 mi)
per day. An ACM can bulge up to 20 km (12 mi) and a NP up to 120 km (75 mi)
from the current's mean position. The AC passes 34 km (21 mi) offshore and an
ACM can reach 123 km (76 mi) offshore. When the AC meanders, its width broadens
from 88 km (55 mi) to 125 km (78 mi) and its velocity weakens from 208 cm/s (82
in/s) to 136 cm/s (54 in/s). An ACM induces a strong inshore counter-current.
Large-scale cyclonic meanders known as Natal pulses are
formed as the Agulhas Current reaches the continental shelf on the South
African east-coast (i.e. the eastern Agulhas Bank off Natal). As these pulses
moves along the coast on the Agulhas Bank, they tend to pinch off Agulhas rings
from the Agulhas Current. Such a ring shedding can be triggered by a Natal
pulse alone, but sometimes meanders on the Agulhas Return Current merge to
contribute to the shedding of an Agulhas ring.