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Chapter I Intro & Objectives - SPREP

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PHOENIX ISLANDS PROTECTED AREA MANAGEMENT PLAN<br />

<strong>Chapter</strong> III. Background, 1. Physical Setting of the Islands<br />

Draft 1 March 2007<br />

In the 1980s, four German cruises (Midpac 1 to IV) were undertaken in the Pacific (Line<br />

Islands, Gilbert Islands, Phoenix Islands, and Marshall Islands) (Glasby 2002).<br />

The Phoenix Islands were oriented along the equator and was predominantly influenced by<br />

the westward-flowing Equatorial Current (northern equatorial branch of the South Equatorial<br />

Current (BEN) and south equatorial branch of the South Equatorial Current (BES)) (Tuna and<br />

Billfish Assessment Program 1993). The Phoenix Islands were subject to the El Niño<br />

Southern Oscillation (ENSO) that occurs every two to seven years and lasts for 18 to 24<br />

months. During ENSO events, the westward tradewinds were reduced and variations and<br />

even reversal of the main currents. This deepens the eastern Pacific thermocline.<br />

The Tuna and Billfish Assessment Programme (1993) provided diagrams of the seasonal<br />

changes in major equatorial surface currents around the Phoenix Islands. These are provided<br />

in Figures III-1.11 to III-1.18 below.<br />

Figure III-1.11. Major currents around the Phoenix Islands in MARCH<br />

Including below the surface temperature and current profiles.<br />

(source: Tuna and Billfish Assessment Programme 1993).<br />

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