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Kana et al. 1988. S. Carolina Charleston SLR Case Study

Kana et al. 1988. S. Carolina Charleston SLR Case Study

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WETLANDS TRANSECTS: METHOD AND RESULTS<br />

To d<strong>et</strong>ermine how an accelerated rise in sea level would affect the w<strong>et</strong>lands of <strong>Charleston</strong>,<br />

one needs to know the portions of land at particular elevations and the plant species found at those<br />

elevations. To characterize the study area, we randomly selected and an<strong>al</strong>yzed twelve transects<br />

(sample cross sections, each running <strong>al</strong>ong a line extending from the upland to the water). This<br />

section explains how the data from each transect were collected and an<strong>al</strong>yzed, presents the results<br />

from each transect, and shows how we created a composite transect based on those results.<br />

Data Collection and An<strong>al</strong>ysis<br />

For budg<strong>et</strong>ary and logistic<strong>al</strong> reasons, m had to use representative transacts near, but not<br />

necessarily within, the study area. For example, a limiting criterion was nearness to convenient places<br />

where reliable elevations, or benchmarks, had <strong>al</strong>ready been established. The marshes be- hind<br />

Kiawah Island and Isle of P<strong>al</strong>ms are similar to the marshes behind Sullivans Island, but are more<br />

accessible. As Figure 2-3 shows, <strong>al</strong>l the transacts %ere within 20 km (12 mi) of the study area.<br />

Each transect began at a benchmark located on high ground near a marsh's boundary, and<br />

ended at a tid<strong>al</strong> creek or mud flat, or after covering 300 m (1,000 ft)-whichever came first. The length<br />

of the transacts was limited because of the difficulty of wading through very soft muds. Although this<br />

procedure may have biased the sample somewhat, logistics prevented a more rigorous survey.<br />

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