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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 />

Stoddar and Fosberg (1994) noting the number of paleohoa (ancient lagoon passages) in<br />

Abariringa (Canton), Enderbury, and Orona (Hull) speculated that hurricanes must have been<br />

more frequent in the Central Pacific in the mid-Holocene period.<br />

The Southern Oscillation refers to variations in air pressure between Indonesia and the South<br />

Pacific (Nunn 1994). When air pressure was anomalously high in one area, it was<br />

anomalously low in the other. The measure for this variation is called the Southern<br />

Oscillation Index (SOI). Extremes of SOI values are associated with extreme weather<br />

conditions such as droughts in the central Pacific (including the Phoenix Islands), and<br />

changes in ocean currents and temperatures.<br />

Nunn (1994) illustrated average annual pressure (mbar) at sea level in January and July based<br />

on observations between 1900 and 1939 (see Figure III-1.35 below). The Phoenix Islands<br />

atmospheric pressure of between 1006 mbars in January to 1009 mbars in July.<br />

Figure III-1.35. Average annual atmospheric pressure (mbar) at sea level in January<br />

and July for the central Pacific, including the Phoenix Islands.<br />

(source: Nunn 1994)<br />

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