Tasman sea

Water type: Sea
Connection to the ocean: Pacific Ocean
Climates: Subtropical, Temperate

Mugiliformes - Mullets

Perciformes - Perches

Carangiformes - Jacks

Istiophoriformes - Barracudas

Lamniformes - Mackerel sharks

Carcharhiniformes - Ground sharks

Orectolobiformes - Carpet shark

Elopiformes - Tarpons and tenpounders

Spariformes - Breams and porgies

Myliobatiformes - Stingrays

Scombriformes - Mackerels

Zeiformes - Dories

Tetraodontiformes - Puffers and filefishes

Lophiiformes - Anglerfishes

Heterodontiformes - Bullhead and horn sharks

Lampriformes - Lamprids

Squaliformes - Sleeper and dogfish sharks

Acanthuriformes - Surgeonfishes

Scorpaeniformes - Mail-cheeked fishes

Centrarchiformes - Basses and sunfishes

Mulliformes - Goatfishes

Anguilliformes - Eels and morays

Labriformes - Wrasses

Gadiformes - Cods

Syngnathiformes - Pipefishes and Seahorses

Echinorhiniformes - Bramble sharks

Notacanthiformes - Spiny eels

Gonorynchiformes - Milkfishes

Beryciformes - Sawbellies

Trachichthyiformes - Rughies

Ophidiiformes - Cusk-eels

Gobiesociformes - Clingfishes

Acropomatiformes - Oceanic basses

Beloniformes - Needlefishes

Trachiniformes - Weeverfishes

Blenniiformes - Blennies

Callionymiformes - Dragonets

Holocentriformes - Squirrelfishes

Clupeiformes - Herrings

Gobiiformes - Gobies

Aulopiformes - Grinners

The Tasman Sea is a marginal sea of the South Pacific Ocean, situated between Australia and New Zealand. It measures about 2,000 km (1,200 mi) across and about 2,800 km (1,700 mi) from north to south. The sea was named after the Dutch explorer Abel Janszoon Tasman, who in 1642 was the first known person to cross it.

The Tasman Sea is informally referred to in both Australian and New Zealand English as the Ditch; for example, crossing the Ditch means travelling to Australia from New Zealand, or vice versa.

Climate
The south of the sea is passed over by depressions going from west to east. The northern limit of these westerly winds is near to 40°S. During the southern winter, from April to October, the northern branch of these winds from the west changes its direction toward the north and goes up against trade winds. Hence, the sea receives frequent winds from the southwest during this period. In the Australian summer (from November to March), the southern branch of the trade winds goes up against west winds and produces further wind activity in the area.

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