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Coastal Impacts, Adaptation, and Vulnerabilities - Climate ...

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84 <strong>Coastal</strong> <strong>Impacts</strong>, <strong>Adaptation</strong>, <strong>and</strong> <strong>Vulnerabilities</strong>During disasters, states <strong>and</strong> municipalities rely extensively on mutual aid agreementswith other jurisdictions, spreading the financial footprint of extreme weather events farbeyond the directly impacted communities. With more frequent events, communitieshave a greater likelihood of having to respond to multiple events simultaneously, overtaxingthese mutual-aid agreements <strong>and</strong> other emergency-response systems <strong>and</strong> funding(Washington Department of Ecology, 2006).Recovery from weather-related extreme events, including those exacerbated by climatechange, is a complicated, long-term process involving virtually every aspect of acommunity’s social <strong>and</strong> economic fabric (see section 4.2). As with response, more intense<strong>and</strong>/or frequent events will lead to more damages <strong>and</strong> thus require more resourcesfor recovery, which will divert those resources from other community functions <strong>and</strong> potentiallystifle economic growth. For example, although the construction sector benefitsfrom engagement in post-disaster rebuilding, the funds <strong>and</strong> workers supporting reconstructionare not available to new-building <strong>and</strong> infrastructure projects, limiting the communityor state’s economic growth potential (University of Maryl<strong>and</strong>, 2007). Althoughinsurance is a vital resource to fund recovery from disasters (see Section 4.4.6), it doesnot cover all losses; the balance is borne by the public sector at Federal, state, <strong>and</strong> locallevels, the private sector, <strong>and</strong> individuals.<strong>Coastal</strong> <strong>and</strong> Nearshore Oil <strong>and</strong> GasAs climate change intensifies during the coming decades, changes in marine <strong>and</strong> coastalsystems are likely to affect the potential for energy resource development in the coastalzone <strong>and</strong> the Outer Continental Shelf (OCS). The capacity for exp<strong>and</strong>ing <strong>and</strong> maintainingonshore <strong>and</strong> offshore support facilities <strong>and</strong> transportation networks is also likely tobe affected. The relative importance of climate variables <strong>and</strong> impacts to the energy sectorwill vary among regions <strong>and</strong> the context in which they are considered, <strong>and</strong> perspectiveson the relative importance of climate change impacts will differ among those whoare responsible for developing adaptation strategies in sectors ranging from industry toregulatory (Burkett, 2011).In this section we summarize the potential energy-sector impacts <strong>and</strong> adaptation effortswith respect to the following climate drivers: temperature change, sea-level rise,<strong>and</strong> changes in storm surge <strong>and</strong> wave patterns. <strong>Climate</strong> change impacts can cascadeamong different oil <strong>and</strong> gas facilities <strong>and</strong> operations from exploration to processing <strong>and</strong>transportation in a way that is similar to the cascading effects that have been observed inmany ecosystems with interactions <strong>and</strong> outcomes that are difficult to predict without apurposeful assessment that considers all relevant drivers (Burkett, 2011).Warming of the ocean can propagate into seafloor sediments. Methane clathrates occuron the continental shelf both in deep sedimentary structures <strong>and</strong> as outcrops on theocean floor. They are common in relatively shallow shelf sediments of the Arctic Ocean<strong>and</strong> the Gulf of Mexico continental slope. The stability of methane clathrate in marinesediments is controlled by the combination of pressure <strong>and</strong> temperature. Seafloor carbonatedeposits reveal several ancient hydrate dissociation events that appear to haveoccurred in connection with rapid global warming events (Archer, 2007; Dickens, 2001;Sassen et al., 2002). Clathrate instability may lead to problems for oil <strong>and</strong> gas exploration<strong>and</strong> development operations ranging from pipeline emplacement to the anchoring of

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