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The hottest product hope you brought beer and dog treats all over print doormat

change in atmospheric CO2 concentration, indicated by the fraction of cumulative CO2 emissions remaining in the atmosphere (dotted lines in Figure 1.4c). Others may depend on the rate of change of GMST, while ‘time-integrated impacts’, such as sea level rise, shown in Figure 1.4d continue to increase even after GMST has stabilised. In this category of 1.5°C pathways, human-induced warming either rises monotonically to stabilise at 1.5°C (Figure 1.4, brown lines) or peaks at or below 1.5°C and then declines . Figure 1.4b demonstrates that pathways remaining below 1.5°C require net annual CO2 emissions to peak and decline to near zero or below, depending on the long-term The hottest product hope you brought beer and dog treats all over print doormatemissions to zero corresponds to stabilizing cumulative CO2 emissions (Figure 1.4c, solid lines) and falling concentrations of CO2 in the atmosphere (Matthews and Caldeira, 2008; Solomon et al., 2009)116, which is required to stabilize GMST if non-CO2 climate forcings are constant and positive. Stabilizing atmospheric greenhouse gas concentrations would result in continued warming (see Section 1.2.4). Total warming refers to the actual

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