The representation of aerosol–cloud interaction in global climate models (GCMs) remains a large s...
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The CH4 growth rate in the atmosphere showed large variations after the Pinatubo eruption in...
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The growth rate of methane (CH4) showed fluctuations in the 1990s, with particularly large&n...
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The global methane (CH4) growth rate showed large variations after the eruption of Mount Pinatubo...
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