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Trend of Surface Air Temperature in Eastern China and Associated Large-Scale Climate Variability over the Last 100 Years

机译:中国东部近100年地表气温变化趋势及相关的大气候变化

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Using the reconstructed continuous and homogenized surface air temperature (SAT) series for 16 cities across eastern China (where the greatest industrial developments in China have taken place) back to the nineteenth century, the authors examine linear trends of SAT. The regional-mean SAT over eastern China shows a warming trend of 1.52 degrees C (100 yr)(-1) during 1909-2010. It mainly occurred in the past 4 decades and this agrees well with the variability in another SAT series developed from a much denser station network (over 400 sites) across this part of China since 1951. This study collects population data for 245 sites (from these 400+ locations) and split these into five equally sized groups based on population size. Comparison of these five groups across different durations from 30 to 60 yr in length indicates that differences in population only account for between 9% and 24% of the warming since 1951. To show that a larger urbanization impact is very unlikely, the study additionally determines how much can be explained by some large-scale climate indices. Anomalies of large-scale climate indices such as the tropical Indian Ocean SST and the Siberian atmospheric circulation systems account for at least 80% of the total warming trends.
机译:利用重建于19世纪的中国东部16个城市(中国发生了最大的工业发展)的重建的连续且均匀的地面气温(SAT)系列,作者检验了SAT的线性趋势。在1909-2010年期间,中国东部地区平均SAT值显示出1.52摄氏度(100年)(-1)的变暖趋势。它主要发生在过去的40年中,这与从1951年以来在中国这一地区的更密集的站点网络(400多个站点)开发的另一个SAT系列的变异性非常吻合。这项研究收集了245个站点的人口数据(从这些站点400多个地点),并根据人口数量将其分为五个大小相等的组。比较这五个小组在30到60年的不同持续时间中的变化,发现人口差异仅占1951年以来变暖的9%到24%。为了显示更大的城市化影响是不太可能的,该研究还确定了多少可以用一些大规模的气候指数来解释。诸如热带印度洋海温和西伯利亚大气环流系统之类的大规模气候指数的异常至少占总变暖趋势的80%。

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