Cloudy

absorption m upper atmosphere mainly by ozone (-3 units)

absorption m tower almos by water vapour ano C (-10 units)

absorption m tower almos by water vapour ano C (-10 units)

reflection from clouds to space M 5 units)

absorption in clouds (-10 units I

reflection from clouds to space M 5 units)

Figure 6.3 Diagram to illustrate the effect of the atmosphere on the radiation budget of the ocean. The values are very approximate and represent average conditions; for example, in absorption in clouds (-10 units I

low latitudes as much as 40% of incoming solar

Mums1

25 units radiation may be absorbed by the atmosphere over the oceans.

reach ocean reach ocean

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