The Tasman Front is a relatively warm water east-flowing surface current and thermal boundary that separates the
Coral Sea to the north and the
Tasman Sea to the south.
Naming
The name was proposed by Denham and Crook in 1976,[1] to describe a thermal front that extends from
Australia and
New Zealand between the Coral Sea and Tasman Sea.[2][3]
Geography
Originating in the edge of the
East Australian Current (EAC), the Tasman Front
meanders eastward between longitudes 152° E and 164° E and latitudes 31° S and 37° S,[4][5] then reattaches to the coastline at New Zealand, forming the East Auckland Current.[6]
Topography plays a dominant role in establishing the Tasman Front.[2] Data on the Tasman Front shows that the path of the front is influenced in part by the forcing of the flow over the major ridge systems.[7] Meanders observed in the Tasman Front can be driven by
meridional flows along ridges such as those observed at the New Caledonia Trough (166° E) and the
Norfolk Ridge (167° E).
Abyssal currents also drive meanders associated with the
Lord Howe Rise (161° E) and Dampier Ridge (159° E).[8]
Oceanography
There have been a number of observational[5][7] and modeling[8][9] studies on this front in addition to a number of paleo-oceanographic studies of marine sediments.[10] Contrarily, there have been few biological observational studies, but those have been conducted resulted in relating the physical features of the front to properties of fish communities.[11] Likewise, there are even fewer studies relating biogeochemical properties to physical processes of the Tasman Front.[3]
^
abBaird, Mark E.; Timko, Patrick G.; Middleton, Jason H.; Mullaney, Thomas J.; Cox, Deborah R.; Suthers, Iain M. (November 2008). "Biological properties across the Tasman Front off southeast Australia". Deep-Sea Research Part I: Oceanographic Research Papers. 55 (11): 1438–1455.
Bibcode:
2008DSRI...55.1438B.
doi:
10.1016/j.dsr.2008.06.011.
^Griffiths, F. B.; Wadley, V. A. (November 1986). "A synoptic comparison of fishes and crustaceans from a warm-core eddy, the East Australian Current, the Coral Sea and the Tasman Sea". Deep-Sea Research Part A: Oceanographic Research Papers. 33 (11): 1907–1922.
Bibcode:
1986DSRA...33.1907G.
doi:
10.1016/0198-0149(86)90085-3.