《Table 4 Trends in seasonal average air temperature for three geographic zones in China》

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《中国气温变化对全球变暖停滞的响应（英文）》

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Beyond the seasonal differences during the warming hiatus across China，there are differences across the three geographic zones.Table 4 shows the trends in air temperature for three geographic zones across different seasons and periods.Slowed warming in the eastern monsoon region is mainly reflected in changes in winter air temperature，whose trends were–0.896℃/10a in winter and 0.134℃/10a in summer for 1998–2012.In the northwestern arid region，the trend magnitudes were–1.425℃/10a in winter and 0.217℃/10a in summer for1998–2012.The air temperatures in spring and autumn showed insignificant cooling trends.In high frigid region of the Tibetan Plateau，the warming rate was 0.337℃/10a in summer during 1998–2012，lower in spring and winter，and autumn showed a slight cooling trend.In summary，winter contributed the most to the warming hiatus and summer had the smallest contribution in eastern and northwestern China.In addition，temperature increases were the fastest in summer on the Tibetan Plateau.