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Vol. 53 - Alaska Resources Library and Information Services

Vol. 53 - Alaska Resources Library and Information Services

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The approach taken in this analysis is one that considers major life<br />

history stanzas of the species in regards to important biological<br />

<strong>and</strong> ecological traits, <strong>and</strong> discusses the modes <strong>and</strong> extent of oil pollution<br />

as it may affect these stages. Use of life history stanzas is<br />

considered a sound categorical division for comparing <strong>and</strong> contrasting<br />

physiological, reproductive <strong>and</strong> ecological changes that occur during a<br />

life cycle (Wooster 1983). Armstrong, et al. (1983b) have provided a<br />

review of oil impact literature <strong>and</strong> interpreted their data in light of<br />

these life history stanzas. The assertions <strong>and</strong> hypotheses of Armstrong,<br />

et al. (1983b) have been modified in accordance with the field data<br />

acquired during the present study.<br />

4.5.1 Oil Transport Models <strong>and</strong> Impact Scenarios<br />

Before relating the biology of red king crab to predictions of oil<br />

impact, it is important to first discuss the physical transport of oil<br />

both horizontally <strong>and</strong>/or vertically by currents, winds <strong>and</strong> biological<br />

processes. A brief recount of oil impact scenarios used at OCSEAP<br />

synthesis meetings will illustrate the locations <strong>and</strong> magnitude of oil<br />

pollution considered to be representative of possible spills along the<br />

NAS <strong>and</strong> in the St. George Basin. These scenarios will serve as a point<br />

of reference in framing estimates of species' vulnerability based on<br />

data in this report.<br />

Two models of physical transport processes, water movements <strong>and</strong> biological<br />

interactions <strong>and</strong> responses to oil in the Bering Sea have been<br />

constructed (Leendertse <strong>and</strong> Liu 1981; Sonntag, et al. 1980). Several<br />

models of water transport <strong>and</strong> circulation have been based on net current<br />

directions <strong>and</strong> velocity (Hebard 1959; Kinder <strong>and</strong> Schumacher 1981b), <strong>and</strong><br />

on methane profiles (Cline, et al. 1981).<br />

Hebard (1959) described currents moving to the northwest through Unimak<br />

Pass, with a component then moving northeast along the North Aleutian<br />

Shelf. Although the direction of the current is highly variable <strong>and</strong><br />

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