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EPA's Vessel General Permit and Small Vessel General

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l<strong>and</strong>-uses: rain that would normally infiltrate in forest, grassl<strong>and</strong> <strong>and</strong> wetl<strong>and</strong> soils falls on <strong>and</strong><br />

flows over impervious surfaces. That runoff is then channeled into storm sewers <strong>and</strong> released<br />

directly into surface waters (rivers <strong>and</strong> streams), which changes the magnitude <strong>and</strong> variability of<br />

water velocity <strong>and</strong> volume in those receiving waters.<br />

Aquatic Nuisance Species<br />

Aquatic nuisance species (ANS) are aquatic <strong>and</strong> terrestrial organisms, introduced into new<br />

habitats throughout the United States <strong>and</strong> other areas of the world, that produce harmful impacts<br />

on aquatic natural resources in these ecosystems <strong>and</strong> on the human use of these resources<br />

(http://www.anstaskforce.gov). They are also referred to as invasive, alien, or nonindigenous<br />

species. Introduction of these species is cited as a major threat to biodiversity, second only to<br />

habitat loss (Wilcove et al. 1998). They have been implicated in the endangerment of 48% of the<br />

species listed under ESA (Czech <strong>and</strong> Krausman 1997). In Hawai’i, 343 marine aquatic invasive<br />

species have been documented. Over 250 nonindigenous species of invertebrates, algae, <strong>and</strong><br />

microorganisms have established themselves in the coastal marine ecosystems of California,<br />

whose waters have been the subject of most in-depth analyses of aquatic invasions in the U.S.<br />

More than 180 invaders have been detected <strong>and</strong> described in the Great Lakes, which are among<br />

the best-studied freshwater systems in the world.<br />

Climate Change<br />

All species discussed in this Opinion are or will be threatened by the direct <strong>and</strong> indirect effects of<br />

global climatic change. There is now widespread consensus within the scientific community that<br />

atmospheric temperatures on earth are increasing (warming) <strong>and</strong> that these increases will<br />

continue for at least the next several decades (IPCC 2001b). The Intergovernmental Panel on<br />

Climate Change (IPCC) estimated that average global l<strong>and</strong> <strong>and</strong> sea surface temperature has<br />

increased by 0.6°C (± 0.2) since the mid-1800s, with most of the change occurring since 1976.<br />

This temperature increase is greater than what would be expected given the range of natural<br />

climatic variability recorded over the past 1,000 years (Crowley <strong>and</strong> Berner 2001). The IPCC<br />

reviewed computer simulations of the effect of greenhouse gas emissions on observed climate<br />

variations that have been recorded in the past <strong>and</strong> evaluated the influence of natural phenomena<br />

such as solar <strong>and</strong> volcanic activity. Based on their review, the IPCC concluded that natural<br />

phenomena are insufficient to explain the increasing trend in l<strong>and</strong> <strong>and</strong> sea surface temperature,<br />

<strong>and</strong> that atmospheric warming observed over the last 50 years is probably attributable to human<br />

activities (IPCC 2001b). Climatic models estimate that global temperatures would increase<br />

between 1.4 to 5.8°C from 1990 to 2100 if humans do nothing to reduce greenhouse gas<br />

emissions from current levels (IPCC 2001b).<br />

In the Northeast, annual average temperatures have increased by 2°F since 1970, with winter<br />

temperatures increasing by up to 4°F (Karl et al. 2009). Over the same time interval, the<br />

Northeast has experienced more days with temperatures greater than 90°F, a longer growing<br />

season, increased heavy precipitation, more winter precipitation falling as rain than as snow,<br />

reduced snowpack, earlier breakup of winter ice on lakes <strong>and</strong> rivers, earlier spring snowmelt<br />

resulting in earlier peak river flows, rising sea surface temperatures <strong>and</strong> sea level.<br />

Over the next several decades, the Northeast is expected to experience temperatures increases of<br />

205

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