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in lots of parts of the Northern Hemisphere. The effects have been especially severe within the northeastern United States, with common temperatures in New England as much as 3.5 °C below regular in June, as an example, and unseasonal frosts and snowfalls. Europe was additionally badly affected, resulting in crop failures and famine in England, France and Germany. The below-average temperatures lasted for about two years. We come now to our last refinement to the easy image in Figure 7. Recall that the troposphere is heated from under, with temperature then falling with rising altitude. This situation units the scene for the onset of convection – the bulk circulate or circulation of a fluid driven by variations in temperature. Convection in the atmosphere plays a vital function in two further mechanisms – quite apart from the emission of longwave radiation – whereby vitality is transferred from the Earth’s surface to the environment. About half of the incoming near-infrared radiation can be absorbed, mainly by water vapour low down within the troposphere. In addition, the environment contains a huge assortment of aerosols – fantastic stable particles and liquid droplets suspended within the air. Except in the aftermath of a significant volcanic eruption (of which more in Section 1.5), aerosols are additionally most plentiful in the decrease atmosphere; pure sources embody desert mud wafted into the air by wind, smoke and soot from wildfires, salt from sea-spray, and so forth. Depending on their make-up, aerosols can take in solar radiation – or scatter a few of it back to house. Globally, aerosols make a big contribution to the Earth’s albedo (included within the figure of 31% quoted earlier). They also play another important function. Many aerosols act as cloud condensation nuclei, providing surfaces that promote the condensation of water vapour to form the liquid droplets suspended in clouds – a course of that occurs less readily in ‘clean’ (i.e. aerosol-free) air. Taken together, the pure greenhouse gases take in infrared wavelengths throughout a

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