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3.0 Affected Environment - Knik Arm Bridge and Toll Authority

3.0 Affected Environment - Knik Arm Bridge and Toll Authority

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<strong>Knik</strong> <strong>Arm</strong> Crossing DraftFinal EIS<br />

<strong>Affected</strong> <strong>Environment</strong><br />

Creek, producing <strong>and</strong> exporting plant material, <strong>and</strong> providing limited wildlife habitat. The<br />

sedge wetl<strong>and</strong> adjacent to a pond may provide resting <strong>and</strong> staging habitat for migratory<br />

waterfowl; however, habitat quality is limited in this urban environment.<br />

3.8.3 Floodplains<br />

Floodplains are defined in EO 11988 as “the lowl<strong>and</strong> <strong>and</strong> relatively flat areas adjoining<br />

inl<strong>and</strong> <strong>and</strong> coastal waters including floodprone areas of offshore isl<strong>and</strong>s, including at a<br />

minimum, that area subject to a one percent or greater chance of flooding in any given year”<br />

(Federal Register 1977). EO 11988 directs federal agencies, <strong>and</strong> the activities undertaken or<br />

authorized by them, to reduce the risk of flood loss <strong>and</strong> to minimize flood impacts to human<br />

inhabitants of an area. Additionally, a location hydraulic study (KABATA 2006c) has been<br />

prepared in accordance with 23 C.F.R. 650 Subpart A, to assess impacts from encroachments<br />

associated with implementation of the proposed KAC project.<br />

3.8.3.1 The Mat-Su<br />

The Federal Emergency Management Agency (FEMA) has mapped base flood elevations<br />

(i.e., 100-year flood elevations) along the Little Susitna River <strong>and</strong> Lucile Creek within the<br />

Mat-Su; however, FEMA maps are not available for the majority of the Mat-Su portion of the<br />

Study corridor. Unmapped floodplains exist within the Goose Creek tributaries <strong>and</strong> closeddrainage<br />

lakes along the Study corridor. Floodplain areas associated with these water bodies<br />

are small in area <strong>and</strong> immediately adjacent to the creek or lake.<br />

Inundation of these floodplains is generally associated with spring snowmelt or large<br />

precipitation events. Because the drainage basin of each water body is small, precipitation<br />

events that cause flooding are localized to the immediate area around the water body.<br />

Flooding adjacent to the creeks has a short duration because the creeks can drain quickly.<br />

Flooding in the closed-drainage lakes lasts longer because the lakes have no stream outlet<br />

<strong>and</strong> the water must percolate into the ground to dissipate. A detailed flood study would be<br />

required to determine the actual possible flood extents, but it is likely that most of these<br />

flood-prone areas are within 100 feet of either side of the stream bank or lakeshore.<br />

3.8.3.2 <strong>Knik</strong> <strong>Arm</strong><br />

The <strong>Knik</strong> <strong>Arm</strong> shoreline within Anchorage is subject to tidal flooding <strong>and</strong> is mapped as base<br />

floodplain Zone A. This zonal type designates areas where the base flood elevations have not<br />

been determined. However, based on FEMA (2002) data, the Municipality of Anchorage<br />

established <strong>and</strong> regulates the coastal base flood elevation as 19 feet above its datum for<br />

coastal areas of <strong>Knik</strong> <strong>Arm</strong> north of Anchorage. This base flood elevation is approximately<br />

36.4 feet relative to MLLW.<br />

Flooding within these areas is associated with storm events, including high winds (but not<br />

waves) <strong>and</strong> extremely low atmospheric pressure. Inundated areas during these floods include<br />

nearshore lowl<strong>and</strong>s <strong>and</strong> creek <strong>and</strong> river estuaries. Flood duration is short because the flood<br />

peak is associated with high tide.<br />

12/18/07 3-181

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