Source waters of the Pacific Equatorial Undercurrent

Mizuki Tsuchiya, Roger Lukas, Rana A Fine, Eric Firing, Eric Lindstrom

Research output: Contribution to journalArticle

192 Citations (Scopus)

Abstract

Hydrographic and direct current measurements were made north and east Papua New Guinea in June-August 1985 and January-February 1986 as part of the Western Equatorial Pacific Ocean Circulation Study (WEPOCS). Analyses of the data indicate that the major portion of the water in the Equatorial Undercurrent at its beginning north of Papua New Guinea is supplied from the south by a narrow western boundary undercurrent (New Guinea Coastal Undercurrent) transporting high-salinity, low-tritium, high-oxygen, low-nutrient water from the Solomon Sea northwestward along the north coast of Papua New Guinea through the Vitiaz Strait. The New Guinea Coastal Undercurrent has a maximum speed of 40-70 cm s-1 at a depth of about 200 m. It is a permanent feature despite the reversals of the wind and the surface current during the period of the northwest monsoon in austral summer. Its transport through the Vitiaz Strait is as high as 8 × 106 m3 s-1, which is of the same magnitude as the Equatorial Undercurrent transport at 143°E. The New Guinea Coastal Undercurrent revealed by the WEPOCS data is consistent with the low-latitude equatorward western boundary current implied in a calculation of the Sverdrup transport based on the observed wind-stress distribution for the tropical Pacific Ocean. High-salinity, low-tritium, low-oxygen, high-nutrient water which flows westward into the Bismarck Sea passing north of the Solomon Islands is entrained into the Equatorial Undercurrent north of New Ireland and returns to the east, resulting in a down-stream increae in the Undercurrent transport. Low-salinity, high-tritium, high-nutrient water of eastern North Pacific origin also contributes to the Equatorial Undercurrent in its source area west of the WEPOCS region. However, there is no evidence that northern waters are being continuously entrained into the Undercurrent in the WEPOCS region.

Original languageEnglish (US)
Pages (from-to)101-147
Number of pages47
JournalProgress in Oceanography
Volume23
Issue number2
DOIs
StatePublished - 1989

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undercurrent
Pacific Ocean
tritium
New Guinea
Papua New Guinea
salinity
nutrients
water
oxygen
Solomon Islands
North Sea
Ireland
water flow
strait
nutrient
Sverdrup transport
coasts
western boundary current
summer
wind stress

ASJC Scopus subject areas

  • Aquatic Science
  • Geology
  • Oceanography

Cite this

Source waters of the Pacific Equatorial Undercurrent. / Tsuchiya, Mizuki; Lukas, Roger; Fine, Rana A; Firing, Eric; Lindstrom, Eric.

In: Progress in Oceanography, Vol. 23, No. 2, 1989, p. 101-147.

Research output: Contribution to journalArticle

Tsuchiya, M, Lukas, R, Fine, RA, Firing, E & Lindstrom, E 1989, 'Source waters of the Pacific Equatorial Undercurrent', Progress in Oceanography, vol. 23, no. 2, pp. 101-147. https://doi.org/10.1016/0079-6611(89)90012-8
Tsuchiya, Mizuki ; Lukas, Roger ; Fine, Rana A ; Firing, Eric ; Lindstrom, Eric. / Source waters of the Pacific Equatorial Undercurrent. In: Progress in Oceanography. 1989 ; Vol. 23, No. 2. pp. 101-147.
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