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作 者:QIAN WeiHong LU Bo LIANG HaoYuan
出 处:《Chinese Science Bulletin》2011年第3期319-324,共6页
摘 要:Relationships on interannual and interdecadal timescales among global mean air temperature,CO2 concentrations and fossil-fuel carbon emissions in four major developed countries (the United States,the United Kingdom,France,and Germany) were analyzed.On an interannual timescale,the United States fossil-fuel carbon emissions tend to increase during cold winters and decrease during warm winters,which is opposite to the situation in summer.On an interdecadal timescale,cold (warm) periods both in the United States and globally agree with high (low) periods of fossil-fuel carbon emissions,with the temperature variability leading by 5–7 years.The leading correlation on the interdecadal timescale and the asymmetry in seasonal correlation on the interannual timescale indicate that temperature variability is a possible cause of changes in fossil-fuel carbon emissions.Relationships on interannual and interdecadai timescales among global mean air temperature, CO2 concentrations and fossil-fuel carbon emissions in four major developed countries (the United States, the United Kingdom, France, and Germany) were ana- lyzed. On an interannual timescale, the United States fossil-fuel carbon emissions tend to increase during cold winters and de- crease during warm winters, which is opposite to the situation in summer. On an interdecadal timescale, cold (warm) periods both in the United States and globally agree with high (low) periods of fossil-fuel carbon emissions, with the temperature variability leading by 5-7 years. The leading correlation on the interdecadal timescale and the asymmetry in seasonal correlation on the interannual timescale indicate that temperature variability is a possible cause of changes in fossil-fuel carbon emissions.
关 键 词:年际时间尺度 碳排放量 化石燃料 年代际 温度 变率 反应 全球平均气温
分 类 号:P425.42[天文地球—大气科学及气象学] TK018[动力工程及工程热物理]
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