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Global warming and ocean stratification: a potential result of large extraterrestrial impacts

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Figure

Table 1. Description of Ensembles; Maximum SWV Perturbation; RF Using Radiative Model of Maycock et al
Figure 1. (a) Evolution of area-averaged surface air temperatures over the ocean (K), with time after the impact event
Figure 2. (a) Latitude-depth cross section of the difference in zonally averaged potential temperature (K), in the top 300 mof the ocean between ensembles P2 (averaged in time between years 1 and 10 after the impact) and P0
Figure 3. (a) Minimum annually averaged temperature change over land (K), between years 0 and 10 after a simulatedimpact calculated using several hundred simulations of the EBM showing the combined effect of aerosol and SWV RF8.The abscissa shows the most

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