Abstract
Anthropogenic climate change could have disastrous consequences for the survival of atolls around the planet. Although atolls have survived past increases in sea levels through the upward growth of corals, future increases in coral mortality due to raising sea temperatures and ocean acidification will probably mean that coral islands will suffer increasing erosion till they eventually disappear. Geomorphological change is unlikely to be linear with most of the change occurring due to high intensity episodic events. Potential future increases in tropical cyclone intensities due to rising sea temperatures are also likely to increase the pace of coastal erosion, further compounding the problem. While a number of adaptation measures are possible, ultimately the only definite path to ensure that islands can survive the death of corals is through the construction of coastal defences, which will become progressively more expensive as the depth of water in front of them continues to increase.
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Notes
- 1.
It should be noted that opinions on the subject sometimes differ, but as we will show in this chapter it appears unlikely that they will be able to adapt in the short term. For some views on this see Hoegh-Guldberg et al. (2011), pp. 1494–1495.
- 2.
Magnan et al. (2011).
- 3.
Mimura et al. (2007) (A chapter within the IPCC 4AR).
- 4.
Mimura et al. (2007) (A chapter within the IPCC 4AR).
- 5.
Lyytimaki and Hilden (2011), pp. 598–612.
- 6.
Bindoff et al. (2007) (A chapter within the IPCC 4AR).
- 7.
Solomon et al. (2007) (A chapter within the IPCC 4AR).
- 8.
Webb and Kench (2010), pp. 234–246.
- 9.
Solomon et al. (2007) (A chapter within the IPCC 4AR).
- 10.
Allison et al. (2009), pp. 1–64.
- 11.
Allison et al. (2009), pp. 1–64.
- 12.
This research was done by linking sea-level variations on time scales of decades to centuries to the global temperature, which could explain around 98 % of the variance in the data. See Vermeer and Rahmstorf (2009).
- 13.
Magnan et al. (2011).
- 14.
USACE (2011).
- 15.
Though the report does not specify which peer-reviewed articles, thus meaning that the latest research on the subject should be used. An extreme case could be for example the scenarios outlined by Vermeer and Rahmstorf (2009).
- 16.
USACE (2011).
- 17.
Stern (2006).
- 18.
Wassmann et al. (2004), pp. 89–107.
- 19.
Caron (1990), pp. 621–653.
- 20.
- 21.
Mimura et al. (2007) (A chapter within the IPCC 4AR).
- 22.
- 23.
Though the literature on this tends to refer to islands that have already seen violent conflicts for the last decades anyway, such as Solomon Islands and places in Papua New Guinea, see Maas and Carius (2012), pp. 1–17.
- 24.
Barnett (2004), pp. 191–215.
- 25.
- 26.
Climate Prediction Centre (2005).
- 27.
Climate Prediction Centre (2005).
- 28.
Johnson (2011).
- 29.
Kench et al. (2009), pp. 180–213.
- 30.
Reaser et al. (2000), pp. 1500–1511.
- 31.
Burke et al. (2011).
- 32.
Burke et al. (2011).
- 33.
Burke et al. (2011).
- 34.
Burke et al. (2011).
- 35.
Yamano et al. (2011).
- 36.
Yamano et al. (2011).
- 37.
Kench et al. (2009), pp. 180–213.
- 38.
Burke et al. (2011).
- 39.
Reaser et al. (2000), pp. 1500–1511.
- 40.
Kench et al. (2009), pp. 180–213.
- 41.
Kench et al. (2009), pp. 180–213.
- 42.
Kench et al. (2009), pp. 180–213
- 43.
Kench et al. (2009), pp. 180–213.
- 44.
Kench et al. (2009), pp. 180–213.
- 45.
Done (1992), pp. 121–132.
- 46.
Kench et al. (2009), pp. 180–213.
- 47.
Kench et al. (2009), pp. 180–213.
- 48.
- 49.
- 50.
- 51.
Burke et al. (2011).
- 52.
Kleypas and Gattuso (2010).
- 53.
Kleypas et al. (1999), pp. 118–120.
- 54.
Kench et al. (2009), pp. 180–213.
- 55.
Secretariat of the Convention on Biological Diversity (2009), pp. 1–61.
- 56.
Burke et al. (2011).
- 57.
International Society for Reef Studies (2008).
- 58.
Burke et al. (2011).
- 59.
Secretariat of the Convention on Biological Diversity (2009), pp. 1–61.
- 60.
- 61.
Secretariat of the Convention on Biological Diversity (2009), pp. 1–61.
- 62.
Fabricius et al. (2011), pp. 165–169.
- 63.
Fabricius et al. (2011), pp. 165–169.
- 64.
Rogers and Laffoley (2011), pp. 1–18.
- 65.
Veron et al. (2009), pp. 1428–1436.
- 66.
Westmacott et al. (2000).
- 67.
According to JICA (2011).
- 68.
Similar problems exist in other atolls such as Kiribati, according to Loughry and McAdam (2008).
- 69.
Burke et al. (2011).
- 70.
- 71.
Barnett and Adger (2003), p. 325.
- 72.
Caron (1990), pp. 621–653.
- 73.
Kench et al. (2009), pp. 180–213.
- 74.
Kench et al. (2009), pp. 180–213.
- 75.
Kench et al. (2009), pp. 180–213.
- 76.
Kench et al. (2009), pp. 180–213.
- 77.
Kench et al. (2009), pp. 180–213.
- 78.
Vermeer and Rahmstorf (2009).
- 79.
Kench et al. (2009), pp. 180–213.
- 80.
Vermeer and Rahmstorf (2009).
- 81.
Veron et al. (2009), pp. 1428–1436.
- 82.
Yamano et al. (2011).
- 83.
Rogers and Laffoley (2011), pp. 1–18.
- 84.
Veron et al. (2009), pp. 1428–1436.
- 85.
Veron et al. (2009), pp. 1428–1436.
- 86.
The Earth’s orbit around the Sun is elliptical, and thus the effect of the Sun on the tidal range will vary throughout the year.
- 87.
Rakova (2009).
- 88.
According to JICA (2011).
- 89.
Maclellan (2009).
- 90.
Rakova (2009).
- 91.
Displacement Solutions (2009), p. 18.
- 92.
Rakova (2009).
- 93.
Rakova (2009).
- 94.
Rakova (2009).
- 95.
Rakova (2009).
- 96.
Rakova (2009).
- 97.
This is a type of tropical plant that is grown as a root vegetable and as a leaf vegetable. It can be grown in paddy fields or upland areas.
- 98.
Rakova (2009).
- 99.
Rakova (2009).
- 100.
South Capitol Street 2011.
- 101.
Rakova (2009).
- 102.
Rakova (2009).
- 103.
Rakova (2009).
- 104.
Displacement Solutions (2009), p. 18.
- 105.
Rakova (2009).
- 106.
Displacement Solutions (2009), p. 19.
- 107.
Displacement Solutions (2009), p. 18.
- 108.
Displacement Solutions (2009), p. 18.
- 109.
Redfearn 2011 USA, Papua New Guinea. The documentary was nominated for an Oscar at the 83rd Annual Academy Awards in 2011.
- 110.
Rakova (2009).
- 111.
Rakova (2009).
- 112.
Rakova (2009).
- 113.
Adapted from a table detailing the vulnerability of Small Island States, in Pelling and Uitto (2001).
- 114.
Pelling and Uitto (2001).
- 115.
Pelling and Uitto (2001).
- 116.
This country currently faces many challenges, such as overcrowding, land scarcity and poor urban conditions. Particularly important is the threat posed by sea level rise, as a large amount of the country is situated in the low-lying Ganges-Brahmaputra River Delta. The area is thus at high risk from the effects of storm surges which can lead to the inundation of coastal lands where millions of people live. It has been estimated that half of Bangladesh’s population lives in areas less than 5 m below sea level. See Tasnim (2010).
- 117.
Landsea et al. (2006).
- 118.
- 119.
Shibayama et al. (2009).
- 120.
Tasnim (2010).
- 121.
Shibayama et al. (2009).
- 122.
According to the Disaster Management Centre, as reported by Tasnim (2010).
- 123.
Shibayama et al. (2009).
- 124.
Shibayama et al. (2009).
- 125.
Ahmed (2011).
- 126.
Mimura et al. (2007) (A chapter within the IPCC 4AR).
- 127.
Warner et al. (2009).
- 128.
Imamura and Van To (1997), pp. 71–87.
- 129.
See Munich Re (2009).
- 130.
Maclellan (2009).
- 131.
Maclellan (2009).
- 132.
BBC (2009).
- 133.
Kawai et al. (2008).
- 134.
Kawai et al. (2008).
- 135.
Fitchett (1987), pp. 1–7.
- 136.
Fitchett (1987), pp. 1–7.
- 137.
Fitchett (1987), pp. 1–7.
- 138.
Webb and Kench (2010), pp. 234–246.
- 139.
Nordhaus (2006).
- 140.
Webster et al. (2005), pp. 1844–1846.
- 141.
Elsner et al. (2008), pp. 92–94.
- 142.
See of example Landsea et al. (2006), pp. 452–454.
- 143.
Mousavi et al. (2011), pp. 575–597.
- 144.
Knutson and Tuleya (2004), pp. 2458–2468.
- 145.
- 146.
- 147.
Knutson et al. (2010), pp. 157–163.
- 148.
Knutson et al. (2010), pp. 157–163.
- 149.
Kawai et al. (2008).
- 150.
Mousavi et al. (2011), pp. 575–597.
- 151.
Mousavi et al. (2011), pp. 575–597.
- 152.
- 153.
- 154.
Mendelsohn et al. (2012).
- 155.
Esteban et al. (2013).
- 156.
Stromberg et al. (2011), pp. 1079–1090.
- 157.
Mimura et al. (2007) (A chapter within the IPCC 4AR).
- 158.
Kench et al. (2009), pp. 180–213.
- 159.
Kench et al. (2009), pp. 180–213.
- 160.
Though other events such as volcanic eruptions or landslides also generate them.
- 161.
Mikami et al. (2012), pp. 1–26.
- 162.
- 163.
Maclellan (2009).
- 164.
Fritz et al. (2006), pp. 137–154.
- 165.
An estimated 40 % of the lands in the Maldives were inundated, see Lamb (2005).
- 166.
Fritz et al. (2006), pp. 137–154.
- 167.
Fritz et al. (2006), pp. 137–154.
- 168.
- 169.
Fritz et al. (2006), pp. 137–154.
- 170.
- 171.
- 172.
- 173.
Kunkel et al. (2006).
- 174.
Although there is a general belief that coastal forests can help to protect against a tsunami, it is not always clear whether they actually offer much protection. Moreover, as observed, the forests can often suffer much damage themselves. Indeed, for the stronger events, such as in this case, the tsunami can rip trees and carry them inland, increasing thus the damage to infrastructure. This process can result in greater damage to human settlements, with the trees becoming floating debris that can then hit both structures and individuals.
- 175.
Mikami et al. (2012).
- 176.
Mori et al. (2010), pp. 15–19.
- 177.
Mori et al. (2010), pp. 15–19.
- 178.
Mori et al. (2010), pp. 15–19.
- 179.
Mori et al. (2010), pp. 15–19.
- 180.
Hemer et al. (2010), pp. 475–491.
- 181.
Kench et al. (2009), pp. 180–213.
- 182.
Kench et al. (2009), pp. 180–213.
- 183.
Storlazzi et al. (2011).
- 184.
Storlazzi et al. (2011).
- 185.
Storlazzi et al. (2011).
- 186.
Kench et al. (2009), pp. 180–213.
- 187.
Sheppard et al. (2005), pp. 223–234.
- 188.
Sheppard et al. (2005), p. 224.
- 189.
Sheppard et al. (2005), p. 226.
- 190.
Sheppard et al. (2005), p. 223.
- 191.
Also on the friction of the sediment particles, for more details see Hearn (1999), pp. 30007–30019.
- 192.
Hearn (1999), pp. 30007–30019.
- 193.
Kench and Cowell (2002), pp. 645–656.
- 194.
Kench et al. (2009), p. 201.
- 195.
Webb and Kench (2010), pp. 234–246.
- 196.
Webb and Kench (2010), pp. 234–246.
- 197.
Kench et al. (2009), p. 186.
- 198.
Kench et al. (2009), p. 207.
- 199.
Sato and Yokoki (2010), p. 2.
- 200.
Accretion means the accumulation of sediments in a certain area, i.e. the opposite of erosion.
- 201.
Sato and Yokoki (2010), p. 4.
- 202.
Beach nourishment describes an engineering process by which some sand which is lost (typically due to the longshore transport process, where the waves move the sand along the shore from one place to the next) is replaced with sand which is sourced from a different area. In this way, the shoreline’s profile can be maintained at a certain location.
- 203.
Sato and Yokoki (2010), pp. 1–2.
- 204.
Sato and Yokoki (2010), p. 5.
- 205.
As calculated by Fujita et al. (2009), pp. 29–45.
- 206.
Sato and Yokoki (2010), p. 9.
- 207.
Sato and Yokoki (2010), p. 11.
- 208.
Vermeer and Rahmstorf (2009).
- 209.
Sato and Yokoki (2010), pp. 1–15.
- 210.
The height of waves is generally dependant on depth of the water, with deeper water meaning that higher waves are possible in a given area.
- 211.
Storlazzi et al. (2011), p. 94.
- 212.
Storlazzi et al. (2011), p. 83.
- 213.
Storlazzi et al. (2011), p. 83.
- 214.
According to the CIA (2012).
- 215.
According to the Japan International Cooperation Agency JICA (2011).
- 216.
Fitchett (1987), p. 1.
- 217.
Fitchett (1987), p. 1.
- 218.
According to JICA (2011), p. 4.
- 219.
Islets, or “coral islands” are the inhabitable part of atolls. It is formed from the dead skeleton of corals and foraminifera, and are the only part of the atoll which are above the sea surface. An atoll typically has several islets or “coral islands” on its surface, as seen in Fig. 2.8. Thus, Fongafale Islet is located within the capital atoll of Funafati.
- 220.
Webb (2005), pp. 1–17.
- 221.
JICA (2011), p. 4.
- 222.
JICA (2011), p. 1.
- 223.
Maragos et al. (1973).
- 224.
Webb (2005), pp. 1–17.
- 225.
Webb (2005), pp. 1–17.
- 226.
Webb and Kench (2010).
- 227.
Webb (2005), pp. 1–17.
- 228.
Warmer et al. (2009), p. 9.
- 229.
JICA (2011), p. 5.
- 230.
JICA (2011), p. 5.
- 231.
JICA (2011), p. 8.
- 232.
- 233.
BBC (2011).
- 234.
Maclellan (2009), p. 17.
- 235.
Maas and Carius (2012), p. 655.
- 236.
UNFCCC (2007).
- 237.
Magnan et al. (2011), p. 3.
- 238.
Magnan et al. (2011), p. 3.
- 239.
Maas and Carius (2012), p. 655.
- 240.
Magnan et al. (2011), p. 3.
- 241.
Maclellan (2009), p. 17.
- 242.
The case of Niue is an interesting one, where a typhoon in 2004 devastated the island and transformed the island into a net importer of food for some time, see Maas and Carius (2012), p. 655.
- 243.
Barnett and Campbell (2010), p. 33.
- 244.
Barnett and Campbell (2010), pp. 15–17.
- 245.
Onuma and Arino (2011), pp. 639–656.
- 246.
Barnett and Campbell (2010), p. 9.
- 247.
It is important to stress the strong role that the chief of the villages (which are given the name of “Matai”) plays in a society that has strong social connections, and how such social conditions allow for a quick decision-making process on how to adapt to the results of natural disasters. See Mikami et al. (2011a, b).
- 248.
A village for example might be located in an area where the water flows from gravity from the mountain, and relocating it to the top might remove this water supply and require finding a new one. This in turn raises the problems of watershed managing, the possibility of needing pumps (and the costs involved in operating them, etc.). This information came from the problems faced by a Samoan village trying to relocate after the tsunami, as described in an email response by Kevin Petrini of the United Nations Development Programme (UNDP) to the CCD (Climate Change and Development) Community to the “Providing Additionality in Adaptation Projects – Examples; Experiences” thread. Email in file with authors.
- 249.
Barnett and Campbell (2010), pp. 1–19.
- 250.
Morita (2008), p. 67.
- 251.
Warner et al. (2009), p. 3.
- 252.
Other sources providing adaptation funds or exploring how to do it would include the World Bank, the United Nations Development Programme (UNDP), the Organisation of American States (OAS), Regional Development Banks, or International Financial Institutions (including Swiss RE or Citigroup, for example), the Special Climate Change Fund, or the Least Developed Countries Fund as listed in Warner et al. (2009), pp. 34–35 and Morita (2008), p. 68.
- 253.
Morita (2008), p. 69.
- 254.
A total of US$230 million, according to Morita (2008), p. 70.
- 255.
As commented by Brian Dawson of the Secretariat of the Pacific Community (SPC) to the CCD (Climate Change and Development) Community to the “Providing Additionality in Adaptation Projects – Examples; Experiences” thread. Email in file with authors.
- 256.
As commented by Brian Dawson of the Secretariat of the Pacific Community (SPC) to the CCD (Climate Change and Development) Community to the “Providing Additionality in Adaptation Projects – Examples; Experiences” thread. Email in file with authors.
- 257.
As commented by Brian Dawson of the Secretariat of the Pacific Community (SPC) to the CCD (Climate Change and Development) Community to the “Providing Additionality in Adaptation Projects – Examples; Experiences” thread. Email in file with authors.
- 258.
Warner et al. (2009), p. 27.
- 259.
Warner et al. (2009), p. 28.
- 260.
Between AU $365 and 668 m, according to Maclellan (2009), p. 9.
- 261.
Okubo and Onuma (2010), pp. 69–80.
- 262.
Okubo and Onuma (2010), pp. 69–80.
- 263.
Okubo and Onuma (2010), pp. 69–80.
- 264.
Thomas Cook Travel Inflight Travel Magazine (2012), pp. 94–100.
- 265.
In fact, there is anecdotal evidence how in places like Bangladesh already how farmers in coastal areas are shifting from crop cultivation to crab farming in areas that were once fields, as unless embankments are repaired water can sometimes enter during high tides, see Ahmed (2011).
- 266.
Warner et al. (2009), p. 3.
- 267.
Warner et al. (2009), p. 33.
- 268.
Warner et al. (2009), p. 34.
- 269.
Warner et al. (2009), p. 33.
- 270.
- 271.
IOM (2008), p. 38.
- 272.
Of course it is also possible to think that migration is actually a failure to adapt to changing weather conditions, though it also has to be understood that humans are not always able to adapt to a changing environment and thus migration is part of the natural adaptation process. Primitive human societies in many areas of the world have been described as hunters-gatherers, constantly moving in a nomadic fashion from one area to the next. Thus, migration appears as a natural way in which humans adapted to changes in their environment.
- 273.
McAdam (2011), pp. 102–137.
- 274.
Philippe Bancour of the IOM on his keynote speak at the “Climate Change and Migration in the South Pacific Region: Policy Perspectives”, organised by the Institute of Policy Studies, Victoria University of Wellington, Wellington, New Zealand, 9-10th July, 2009.
- 275.
Farbotko and Lazrus (2011), p. 7.
- 276.
As mentioned in Loughry and McAdam (2008). The President of the Republic of the Marshall Islands, Jurelang Zedkaia, also mentions relocation as an “undeniable threat” in his keynote address to the “Threatened Island Nations Conference” at Columbia University on the 24 May 2011.
- 277.
Boege (2010), p. 19.
- 278.
Boege (2010), though these statistics should be viewed with caution, as different authors appear to come up with a variety of statistics depending on how these are derived. In fact population in Kiribati has already been moved to the atoll of South Tarawa, which has resulted in over half of the population of Kiribati living there and prompting the government in the 1990s to relocate some 5,000 to outlying atolls, according to Loughry and McAdam (2008).
- 279.
See Farbotko and Lazrus (2011), p. 7.
- 280.
IOM (2007), p. 6.
- 281.
IOM (2007), p. 6.
- 282.
IOM (2007), p. 6.
- 283.
Boege (2010), p. 21.
- 284.
As summarised in Boege (2010).
- 285.
As summarised in Boege (2010).
- 286.
McAdam (2011), pp. 102–137.
- 287.
McAdam (2011), pp. 102–137.
- 288.
McAdam (2011), pp. 102–137.
- 289.
Sinane et al. (2010), para. 3.
- 290.
AOSIS (2008).
- 291.
- 292.
Maclellan (2009), p. 27.
- 293.
Maclellan (2009), p. 23.
- 294.
During a private conversation at Waseda University in the June 2011, Tokyo, Japan.
- 295.
Ewing (2010), pp. 261–286.
- 296.
Ewing (2010), pp. 261–286.
- 297.
- 298.
Mori et al. (2010), p. 17.
- 299.
Not necessarily always, but in general these effects appear to be ignored.
- 300.
This significant wave height is estimated as the average of the top one-third of the waves in a given storm.
- 301.
Esteban et al. (2011).
- 302.
Fifty years was the assumed design life of rubble mound breakwaters, though it should be noted that typically they are designed with a life of 30 years.
- 303.
Vermeer and Rahmstorf (2009).
- 304.
The figure plots the effect that sea level has on different values of water depth (h), for a beach slope θ = 1:30 and a significant wave height outside the barrier reef H s = 9 m.
- 305.
This run-up is defined as the vertical distance above still water which is reached by the waves as they rush up the seaside slope of the structure.
- 306.
Vermeer and Rahmstorf (2009).
- 307.
Taking into account the requirement for increased armour and for the breakwater to be built to a higher level. See Esteban et al. (2011).
- 308.
Okayasu and Sakai (2006), pp. 4883–4893.
- 309.
Takagi et al. (2011), p. 37.
- 310.
The surf zone is the area near the coastline where the waves break. These breaking waves can exert very large forces on structures.
- 311.
Goda (2000), p. 443.
- 312.
Associated with the existence of stress acting on the water due to the presence of wave motion (called radiation stress).
- 313.
The magnitude of the radiation stress may change due to variations in the wave height as it propagates towards the coastline (due to shoaling and wave breaking), and hence this may cause changes in the inclination of the mean water level.
- 314.
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Yamamoto, L., Esteban, M. (2014). Climate Change and Its Effects on Atoll Island States. In: Atoll Island States and International Law. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-38186-7_3
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