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CLIMATE CHANGE AND COASTAL VULNERABILITY IN SMALL ISLAND STATES

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Title: CLIMATE CHANGE AND COASTAL VULNERABILITY IN SMALL ISLAND STATES


1
CLIMATE CHANGE AND COASTAL VULNERABILITY IN SMALL
ISLAND STATES
  • Leonard A. Nurse
  • IPCC Coordinating Lead Author
  • AOSIS Inter-Regional Preparatory Meeting for
    WSSD, January 7 - 11, 2002

2
BACKGROUND AND CONTEXT
  • Consensus of Marine and Coastal Scientists
  • Global climate change will affect the physical,
    biological and biogeochemical characteristics of
    the oceans and coasts, modifying their ecological
    structure, their functions, and the goods and
    services they provide
  • (IPCC-TAR, p. 345, Chapter 6, Coastal Zones and
    Marine Ecosystems).
  • In the case of small islands, coastal
    vulnerability to climate change will be enhanced
    as a consequence of
  • ?Sea-level rise
  • ?Accelerated erosion
  • ?Increased risk of storm flooding and
    inundation
  • ?Elevated sea-surface temperatures

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4
COASTAL VULNERABILITY CONSEQUENCES FOR SMALL
ISLAND STATES
  • Sea-Level Rise
  • Although there are regional variations in the
    signal, sea level in the regions of the Small
    Island States is expected to rise by as much as
    5mm yr-1, for next 100 yrs, as a result of
    GHG-induced global warming. Some of the
    consequences will be
  • ? Coastal Land loss, especially on atolls
    (Pacific and Indian Oceans) and low limestone
    islands (Caribbean).E.g. on Majuro Atoll (Marshal
    Islands), 65 ha (80 dry land) would be lost. In
    extreme cases, abandonment of some atolls and
    small islands may be the only practical option,
    given (i) elevation a.m.s.l., and (ii) physical
    size. E.g. Maldives, Indian Ocean.
  • ?Loss of coastal infrastructure. Practically all
    critical infrastructure is located at or near the
    coast on islands.

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6
COASTAL VULNERABILITY CONSEQUENCES FOR SMALL
ISLAND STATES (contd)
  • Beach Erosion
  • Model runs and observed data consistently project
    that accelerated beach erosion will be an
    inevitable threat facing small islands. While
    much present-day erosion is man-induced (sand
    mining, construction in active beach zone,
    infringement of building set-backs, etc.),
    empirical studies show that SLR is a significant
    contributory factor.
  • ?Higher Water Levels Higher Wave Amplitude
    Increased Wave Energy
  • ? (a) In Trinidad, some beaches are retreating by
    as much as 2.0 m yr-1, where sea level has been
    rising at rate of 8-10 mm yr-1, during the past
    15 years. (b) In Fiji, where sea level has risen
    by 1.0-1.5 mm yr-1, beaches at Viti Levu and
    Taveuni have retreated by some 30.0 m since 1960.

7
CONSEQUENCES OF CLIMATE CHANGE FOR SMALL ISLAND
STATES (contd)
  • Storm Surge, Flood Risks and Inundation
  • Although there is uncertainty about the future
    behaviour of tropical cyclones (hurricanes),
    flood risks and inundation from storm surge will
    be more severe.
  • ?Even quantitatively small increases in relative
    sea level will have a disproportionate effect on
    flood levels (Non-linear relationship between SLR
    and inundation levels).
  • ?Flood risk modeling (HADCM2, HADCM3, UKMO,
    1999) suggests that by 2080, numbers facing
    severe floods in the Caribbean, Indian and
    Pacific Ocean regions would be 200 times higher
    than if there were no SLR.
  • ?Recent studies in Cuba (Perez et al. 1999,
    based on HADCM2), identified 98 coastal
    settlements with a total population exceeding 50
    000 persons, which would be completely inundated
    by a 1.0 m rise in sea-level.

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9
CONSEQUENCES OF CLIMATE CHANGE FOR SMALL ISLAND
STATES (contd)
  • Coral reefs
  • Observational evidence shows that periodic
    warming of the ocean surface, as occurs in El
    Nino years, leads to coral bleaching. The major
    events of the past 20 years occurred at times
    when ocean temperatures have been about 10 C
    higher than the summer maximum.
  • ?Most intense episode on record occurred during
    1997-98 El Nino. On some islands gt90 of live
    reefs affected.
  • ?Increasing atmospheric CO2 is being
    accompanied by similar increases in the oceans.
    This is expected to lead to a reduction in the
    rate of calcification of reef -building corals by
    between 14-30 by 2050.

10
CONSEQUENCES OF CLIMATE CHANGE FOR SMALL ISLAND
STATES (contd)
  • Tourism is a major revenue earner and generates
    significant employment. In addition the industry
    is almost entirely coastal. The impact of
    climate change on this sector will be both direct
    and indirect.
  • SLR will disrupt the sector through loss of
    beaches, the threat to physical plant and vital
    infrastructure.
  • The industry is also sensitive to other
    climate-related impacts, e.g. the loss of corals
    and other marine flora and fauna, which support
    the scuba diving industry.
  • The highest temperature changes are occurring in
    the middle- and high-latitudes. A large of
    tourism is generated by the desire of visitors to
    escape the cold winters of the North. Milder
    winter temperatures in these markets could reduce
    the appeal of islands as tourist destinations.

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13
COASTAL VULNERABILITY REDUCTION IN SIDS GUIDING
PRINCIPLES AND ACTIONS
  • Guiding Principles
  • While we need financial and technical assistance
    to help us reduce our vulnerability to climate
    change, the response and overall strategy must be
    largely designed and implemented by SIDS.
  • In designing our response and adaptation
    strategies we should seek, wherever possible, to
    draw on the experiences, expertise and relevant
    skills of SIDS and other appropriate developing
    countries (Promotion of South-South cooperation).
  • We must also draw on indigenous skills and
    traditional knowledge that have helped to sustain
    many communities in the past.

14
COASTAL VULNERABILITY REDUCTION IN SIDS GUIDING
PRINCIPLES AND ACTIONS (contd)
  • BASIC REQUIREMENTS
  • Inventory of Coastal Resources and Uses
  • Define the nature of these resources (what are
    they Coral reefs? Seagrasses? Offshore sand
    reserves ? Minerals?)
  • Location/ spatial distribution (Where are these
    resources?)
  • Quantification of resources (How much?)
  • Present status/trends Are the beaches eroding or
    accreting? Are fish stocks dwindling or
    expanding?

15
COASTAL VULNERABILITY REDUCTION IN SIDS GUIDING
PRINCIPLES AND ACTIONS (contd)
  • We Need Tools for Reducing Coastal Vulnerability
  • Training in key areas of marine and coastal
    science e.g. oceanography, marine biology,
    fisheries biology, marine geology, coastal
    geomorphology (Capacity Building).
  • Data collection and scientific research at the
    regional and local scales. For example, few SIDS
    have geodetic-controlled tide gauges or
    continuously recording marine meteorological
    stations (Research and Systematic Observation
    UNFCCC Article 5).
  • Downscaling of GCMs to finer resolution (e.g. 50
    km, 25 km), to better facilitate meaningful
    vulnerability assessment at the island scale
    (Capacity building and Transfer of technology).
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