, 2006) reveals that across the world’s tropics, the coastal population is expected to grow by 45% to 1.95 billion people by 2050, while the number of people occupying the inland tropics will grow by 71% to 2.26 billion. However, the total area of inland tropical land is four times that of coastal regions, so tropical population density in 2050 is projected to be 57 km−2 inland and 199 km−2 on coasts. Coastal communities will generate increased local environmental stresses, although improved management may keep some or all of this

increase unrealized. Table 1 presents three averaged projections of the physico-chemical Ceritinib order state of tropical coastal environments in 2050, using three alternative 5-FU solubility dmso scenarios developed by the international community associated with the IPCC to describe different policy approaches to GHG emissions. The business-as-usual (BAU) scenario uses RCP8.5 (Vuuren et al., 2011) which approximates the earlier SRES A1FI scenario (Rogelj et al., 2012), and involves high levels of fossil fuel use and minimal efforts to reduce GHG emissions. It is

the future to which we are currently moving. By 2050, under this scenario, global temperatures will approximate 1.7 °C warmer relative to the year 2000, rising towards 4.0 °C warmer in 2100 (Fig. 3 in Rogelj et al., 2012). The MODERATE scenario, RCP4.5 (similar to SRES B1), involves strenuous efforts to rapidly reduce emissions such that atmospheric concentration of CO2 is stabilized at around 450 ppm by 2100. In 2050, average global temperature under RCP4.5 will approximate 1.2 °C warmer than 2000. In the STRONG scenario, RCP3-PD, human emissions of CO2 fall to very low levels within one or two decades with the outcome that average global temperature approximates 0.8 °C warmer than 2000 in 2050 and begins to decline by 2100. Tropical sea surface temperatures (SST) are approximated from average global air temperature assuming a small time lag due to the relatively higher thermal inertia of sea water. Higher ocean temperatures lead to thermal expansion which combines with increased melting

of land ice to raise sea levels. Box 1.  Modeling effects of climate change on Phloretin fishery production in Raja Ampat The Raja Ampat archipelago is a representative coral reef system, currently rich and productive. We simulated a loss of coral biomass, incrementally reducing the biomass of coral from 100% of its current (2008) value, to 0%. Throughout these simulations, current fishing effort was maintained. The model of Ainsworth et al. (2008) includes mediation effects that simulate non-trophic dependencies in the ecosystem such as the protection from predators offered by coral to fish. For this study, we have added an additional effect to represent space-limited growth of benthic algae: as coral biomass declines, benthic algal productivity increases.