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Chapters 1 - U.S. Fish and Wildlife Service

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Environmental Consequences<br />

are identified that could reduce potential water quality impacts <strong>and</strong> they are also feasible,<br />

practicable, <strong>and</strong> cost-effective, the discharger is required to implement the identified alternative<br />

measures. One effective BMP identified in the General Permit is the use non-toxic <strong>and</strong> less toxic<br />

controls. These include larvicides with very low toxicity that pose very little or no threat to the<br />

environment. USEPA has concluded that microbial larvicides (e.g., Bacillus thuringiensis<br />

israelensis, Bacillus sphaericus) do not pose risks to the environment; <strong>and</strong> methoprene, as used in<br />

vector control programs, does not pose unreasonable risks to the environment (California State<br />

Water Resources Board 2004). Therefore, the current vector control practices being conducted on<br />

the Refuge are not expected to result in any adverse effects to water quality.<br />

Public Use<br />

The pathway that provides access for the public from the Refuge office/visitor contact station to<br />

the observation deck consists of decomposed granite installed along a relatively flat surface. No<br />

signs of erosion along the pathway are evident <strong>and</strong> the pathway continues to provide a firm <strong>and</strong><br />

stable surface, therefore, the continuation of the public use program currently conducted on the<br />

Refuge would have little, if any, effect to water quality in the adjacent wetl<strong>and</strong>s.<br />

5.2.1.7 Effects from Climate Change/Sea Level Rise<br />

Overview<br />

Climate change, especially sea level rise, will significantly alter the existing conditions on the coast,<br />

making coastal intertidal habitats, including the salt marsh habitat protected within the Seal Beach<br />

NWR, some of the most at risk habitats in the world. As sea level rises, intertidal mudflats <strong>and</strong><br />

salt marsh habitat will be converted to subtidal habitat. In addition, decreases in precipitation<br />

could adversely affect the health of the remaining cordgrass <strong>and</strong> other salt marsh vegetation that<br />

depends on some seasonal freshwater input to promote plant vigor.<br />

Although global sea level rise is well-documented, as described in Section 4.2.5.2, there are<br />

currently no clear answers regarding how fast <strong>and</strong> to what extent sea level rise will impact these<br />

existing habitats. This makes it difficult to establish specific long-term management strategies for<br />

protecting this important habitat. We must instead rely on adaptive management to help us<br />

identify measures to insure that coastal intertidal habitat <strong>and</strong> the wildlife it supports can persist at<br />

some level as conditions change.<br />

In an effort to better underst<strong>and</strong> the potential effects of sea level rise on the habitat at the Seal<br />

Beach NWR, the <strong>Service</strong> contracted the application of the Sea Level Affecting Marshes Model<br />

(SLAMM) for the refuge. SLAMM 5.0.1, which accounts for the dominant processes involved in<br />

wetl<strong>and</strong> conversion <strong>and</strong> shoreline modifications during long-term sea level rise, predicts the<br />

changes in tidal marsh area <strong>and</strong> habitat type as a result of sea level rise (Park et al. 1989;<br />

www.warrenpinnacle.com/prof/SLAMM). The primary set of global sea level rise scenarios used<br />

within SLAMM was derived from the work of the IPCC (IPCC 2001) <strong>and</strong> was run using the IPCC<br />

<strong>and</strong> fixed-rate scenarios presented in Table 5-1. These scenarios, which include new information<br />

related to assumptions of one meter <strong>and</strong> 1.5 meters of global sea level rise by the year 2100 (Chen<br />

et al. 2006, Monaghan et al. 2006), indicate that global sea level may be rising progressing more<br />

rapidly than was previously assumed. The A1B maximum (A1B Max) scenario incorporates the<br />

suggestion by Rahmstorf (2007) that a feasible range by 2100 might be 50 cm (19.7 inches) to 140<br />

cm (55.1 inches).<br />

The SLAMM analysis for the Seal Beach NWR also incorporated a number of other factors<br />

including: digital elevation mapping derived from LIDAR <strong>and</strong> ifSAR data from 2003 <strong>and</strong> 1998,<br />

respectively; 2005 wetl<strong>and</strong> boundary data from the National Wetl<strong>and</strong>s Inventory; historic trends in<br />

Draft Comprehensive Conservation Plan 5-7

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