Rd. Pingree et al., WILL DEEP SUBTROPICAL RING STORM PHYSALIA CROSS THE MID-ATLANTIC RIDGE AND REACH AMERICA, Journal of the Marine Biological Association of the United Kingdom, 76(3), 1996, pp. 553-567
A short research cruise was planned to trace the movement of a discret
e body of water in the subtropical eastern North Atlantic Ocean. A sub
tropical ring or deep eddy called STORM was found budding off the Subt
ropical Front (STF) south-west of the Azores. A physical, chemical and
biological survey to depths of 3 . 5 km was made of this 400 km scale
body of water which was spinning cyclonically (anticlockwise). The az
imuthal transport or the amount of water swirling in the eddy was 45 S
v. Storm was 'hooked' with ten drogued Argos buoys and a further five
subsurface Alace floats were deployed. Storm is moving westward at sim
ilar to 3 km a day and is expected to reach the Mid Atlantic Ridge in
rather less than a year unless it is destroyed by typography or reabso
rbed into the Azores Current. With current technology, Storm's evoluti
on and westward progress can be observed and analysed remotely, at a d
istance of similar to 3000 km in the laboratory. Realtime position dat
a means that future sea surveys can be planned.