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failed to demonstrate of the variablity of ozone amounts at varying heights. did not raise doubts about current means of measuring ozone reduction. neglected to underline the complexity in measuring radiative changes. overlooked the distinction between early theories and recent evidence.
a growth in water vapor concentration. a drop in atmospheric absorption of solar radiation. a decrease in other radiative forcings or feedbacks. an increase in atmospheric cooling effect.
forms one of anthropogenic causes of radiative forcings. results in both radiative forcings and radiative feedbacks. can hardly affect atmospheric forcings and feedbacks. makes up a significant type of radiative forcing.
complex operations of feedbacks and forcings distinction between radiative feedbacks and forcings. difficulty in balancing forcing-feedback interactions. impact of cloud formation on global climate.
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