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Table 3.1.1: Earliest <strong>and</strong> latest years respectively at which the threshold temperatures are exceeded in the 41<br />
projections*<br />
SRES<br />
Scenario<br />
1.5C Threshold 2.0C Threshold 2.5C Threshold<br />
Earliest Latest Earliest Latest Earliest Latest<br />
A1B 2023 2050 2038 2070 2053 Later than 2100<br />
A2 2024 2043 2043 2060 2056 2077<br />
B1 2027 2073 2049 Later than 2100 2068 Later than 2100<br />
*NB: In some cases the threshold is not reached prior to 2100, the latest date for which the projections are available.<br />
The potential changes in hurricane <strong>and</strong> tropical storm frequency <strong>and</strong> intensity, sea-level rise (SLR), <strong>and</strong><br />
storm surge incidence are also examined for the Caribbean region. For these variables, existing material in<br />
the literature is examined in order to assess the potential changes affecting the tourist destinations.<br />
3.2. Temperature<br />
Observations from the gridded temperature datasets indicate that mean annual temperatures over <strong>Turks</strong><br />
<strong>and</strong> <strong>Caicos</strong> Isl<strong>and</strong>s have increased at an average rate of 0.12˚C per decade over the period 1960-2006. The<br />
observed increases have been more rapid in SON at the rate of 0.15˚C per decade.<br />
General Circulation Model (GCM) projections from a 15-model ensemble indicate that <strong>Turks</strong> <strong>and</strong> <strong>Caicos</strong><br />
Isl<strong>and</strong>s can be expected to warm by 0.7˚C to 2.0˚C by the 2050s <strong>and</strong> 1.0˚C to 3.3˚C by the 2080s, relative to<br />
the 1970-1999 mean. The range of projections across the 15 models for any one emissions scenario spans<br />
around 1-1.5˚C. Projected mean temperature increase is similar throughout the year.<br />
Regional Climate Model (RCM) projections indicate comparable to higher increases in temperatures over<br />
<strong>Turks</strong> <strong>and</strong> <strong>Caicos</strong> Isl<strong>and</strong>s compared to the GCM ensemble median projections for the A2 scenario. In<br />
particular, RCM simulations driven by ECHAM4 indicate temperature increases that are higher than the<br />
GCM ensemble median projections in all seasons. RCM projections indicate increases of 2.9˚C <strong>and</strong> 2.3˚C in<br />
mean annual temperatures by the 2080s, when driven by the ECHAM4 <strong>and</strong> HadCM3 respectively,<br />
compared with GCM ensemble projections of 2.1-3.3˚C for that period. Temperature increases in JJA <strong>and</strong><br />
SON as projected by the RCM simulation driven by HadCM3 are lower than the lowest GCM ensemble<br />
projections.<br />
The improved spatial resolution in the RCM allows the l<strong>and</strong> mass of the larger Caribbean isl<strong>and</strong>s to be<br />
represented, whilst the region is represented only by ‘ocean’ grid boxes at GCM resolution. L<strong>and</strong> surfaces<br />
warm more rapidly than ocean due to their lower capacity to absorb heat energy, <strong>and</strong> we therefore see<br />
more rapid warming over <strong>Turks</strong> <strong>and</strong> <strong>Caicos</strong> Isl<strong>and</strong>s in RCM projections than in GCMs.<br />
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