IPCC Report.pdf - Adam Curry

Chapter 4Changes in Impacts of Climate Extremes: Human Systems and Ecosystems4.4.9.4. Coastal ErosionCoastal erosion is a significant problem in the Arctic, where coastlinesare highly variable due to environmental forcing (wind, waves, sea levelchanges, sea ice, etc.), geology, permafrost, and other elements(Rachold et al., 2005). For example, the amount of coastal erosion alonga 60 km stretch of Alaska’s Beaufort Sea doubled between 2002 and2007. Jones et al. (2009) considered contributing factors to be meltingsea ice, increasing summer sea surface temperature, sea level rise, andincreases in storm power and associated stronger ocean waves.Increasing coastal retreat will have further ramifications for Arcticlandscapes, including losses in freshwater and terrestrial wildlife habitats,in subsistence grounds for local communities, and in disappearingcultural sites, as well as adverse impacts on coastal villages and towns.In addition, oil test wells may be impacted (Jones et al., 2009). Coastalerosion has also become a problem for residents of Inupiat and on theisland of Sarichev (Russian Federation) (Revich, 2008).Permafrost degradation along the coast of the Kara Sea may lead tointensified coastal erosion, driving the coastline back by up to 2 to 4 mper year (Anisimov and Belolutskaya, 2002; Anisimov and Lavrov, 2004).Coastline retreat poses considerable risks for coastal population centersin Yamal and Taymyr and other littoral lowland areas.Since the early 1950s, when the quality of disaster monitoring andreporting improved in the Pacific Islands region, there has been ageneral increasing trend in the number of disasters reported annually(Hay and Mimura, 2010).Pacific Island Countries and Territories (PICs) exhibit a variety ofcharacteristics rendering generalization difficult (see Table 4-2;Campbell, 2006). One form of PICs is large inter-plate boundary islandsformed by subduction and found in the southwest Pacific Ocean. Thesemay be compared to the Oceanic (or intra-plate) islands which were, orare being, formed over ‘hot spots’ in the Earth’s mantle into volcanichigh islands. Some of these are still being formed and some are heavilyeroded with steep slopes and barrier reefs. Another form of PICs isatolls that consist of coral built on submerging former volcanic highislands, through raised limestone islands (former atolls stranded abovecontemporary sea levels). Each island type has specific characteristics inrelation to disaster risk reduction, with atolls being particularly vulnerableto tropical cyclones, where storm surges can completely inundate themand there is no high ground to which people may escape. In contrast,the inter-plate islands are characterized by large river systems and fertileflood plains in addition to deltas, both of which tend to be heavilypopulated. Fatalities in many of the worst weather- and climate-relateddisasters in the region have been mostly from river flooding (AusAID,2005). Raised atolls are often saved from the storm surge effects of4.4.10. Small Island StatesSmall Island States (SIS) in the Pacific, Indian, and Atlantic Oceans havebeen identified as being among the most vulnerable to climate changeand climate extremes (e.g., UNFCCC, 1992; DSD, 1994; UNISDR, 2005).In the light of current experience and model-based projections, SIS, withhigh vulnerability and low adaptive capacity, have substantial futurerisks (Mimura et al., 2007). Smallness renders island countries at risk ofhigh proportionate losses when impacted by a climate extreme (Pellingand Uitto, 2001; see also Case Study 9.2.9 and Box 3-4).Sea level rise could lead to a reduction in island size (FitzGerald et al.,2008). Island infrastructure, including international airports, roads, andcapital cities, tends to predominate in coastal locations (Hess et al.,2008). Sea level rise exacerbates inundation, erosion, and other coastalhazards; threatens vital infrastructure, settlements, and facilities; andthus compromises the socioeconomic well-being of island communitiesand states (Hess et al., 2008).In 2005, regionally averaged temperatures were the warmest in thewestern Caribbean for more than 150 years (Eakin et al., 2010). Theseextreme temperatures caused the most severe coral bleaching everrecorded in the Caribbean: more than 80% of the corals surveyed werebleached, and at many sites more than 40% died. Recovery from suchlarge-scale coral mortality is influenced by the extent to which coralreef health has been compromised and the frequency and severity ofsubsequent stresses to the system.Table 4-2 | Pacific Island type and exposure to climate extremes. Adapted fromCampbell, 2006.Island TypePlate-Boundary Islands• Large land area• High elevations• High biodiversity• Well-developed soils• River flood plains• Orographic rainfallIntra-Plate (Oceanic) IslandsVolcanic High Islands• Steep slopes• Different stages of erosion• Barrier reefs• Relatively small land area• Less well-developed river systems• Orographic rainfallAtolls• Very small land areas• Very low elevations• No or minimal soil• Small islets surround a lagoon• Shore platform on windward side• Larger islets on windward side• No surface (fresh) water• Ghyben Herzberg (freshwater) lens• Convectional rainfallRaised Limestone Islands• Steep outer slopes• Concave inner basin• Sharp karst topography• Narrow coastal plains• No surface water• No or minimal soilExposure to climate risksThese islands are located in the westernPacific. River flooding is more likely to be aproblem than in other island types. In PapuaNew Guinea, high elevations expose areas tofrost (extreme during El Niño). Most majorsettlements are on the coast and exposed tostorm damage.Because of size these islands have substantialexposure to tropical cyclones, which causethe most damage in coastal areas andcatchments. Streams and rivers are subject toflash flooding. Most islands are exposed todrought. Barrier reefs may ameliorate stormsurge and tsunamis.These islands are exposed to storm surge,‘king’ tides, and high waves. They areexposed to freshwater shortages and drought.Freshwater limitations may lead to healthproblems.Depending on height these islands may beexposed to storm surges and wave damageduring cyclones and storms. They are exposedto freshwater shortages and drought.Freshwater problems may lead to health90,5 xproblems.244,4263