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Effect of data homogenization on estimate of temperature trend: a case of Huairou station in Beijing Municipality

机译:数据均匀化对温度趋势估计的影响-以北京市怀柔站为例

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摘要

Daily minimum temperature (Tmin) and maximum temperature (Tmax) data of Huairou station in Beijing from 1960 to 2008 are examined and adjusted for inhomogeneities by applying the data of two nearby reference stations. Urban effects on the linear trends of the original and adjusted temperature series are estimated and compared. Results show that relocations of station cause obvious discontinuities in the data series, and one of the discontinuities for Tmin are highly significant when the station was moved from downtown to suburb in 1996. The daily Tmin and Tmax data are adjusted for the inhomogeneities. The mean annual Tmin and Tmax at Huairou station drop by 1.377℃ and 0.271℃ respectively after homogenization. The adjustments for Tmin are larger than those for Tmax, especially in winter, and the seasonal differences of the adjustments are generally more obvious for Tmin than for Tmax. Urban effects on annual mean Tmin and Tmax trends are -0.004℃/10 year and -0.035℃/10 year respectively for the original data, but they increase to 0.388℃/10 year and 0.096℃/10 year respectively for the adjusted data. The increase is more significant for the annual mean Tmin series. Urban contributions to the overall trends of annual mean Tmin and Tmax reach 100% and 28.8% respectively for the adjusted data. Our analysis shows that data homogenization for the stations moved from downtowns to suburbs can lead to a significant overestimate of rising trends of surface air temperature, and this necessitates a careful evaluation and adjustment for urban biases before the data are applied in analyses of local and regional climate change.
机译:通过应用附近两个参考站的数据,对北京怀柔站1960年至2008年的每日最低温度(Tmin)和最高温度(Tmax)数据进行了检查和调整。估计并比较了城市对原始温度序列和调整后温度序列线性趋势的影响。结果表明,站点的重新定位在数据系列中引起了明显的不连续性,而1996年将站点从市中心转移到郊区时,Tmin的不连续性之一非常显着。针对不均匀性调整了每日的Tmin和Tmax数据。均质后,怀柔站的年平均Tmin和Tmax分别下降1.377℃和0.271℃。 Tmin的调整幅度大于Tmax的调整幅度,尤其是在冬天,并且Tmin的调整幅度的季节性差异通常比Tmax更为明显。对于原始数据,城市对年平均Tmin和Tmax趋势的影响分别为-0.004℃/ 10年和-0.035℃/ 10年,但对于调整后的数据,它们分别增加至0.388℃/ 10年和0.096℃/ 10年。对于年平均Tmin系列,该增加更为显着。对于调整后的数据,城市对年平均Tmin和Tmax总体趋势的贡献分别达到100%和28.8%。我们的分析表明,从市中心转移到郊区的站点的数据均质化可能会导致高估地表气温的上升趋势,因此有必要在数据应用于本地和区域分析之前仔细评估和调整城市偏差。气候变化。

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  • 来源
    《Theoretical and applied climatology》 |2014年第4期|365-373|共9页
  • 作者单位

    College of Atmospheric Science, Nanjing University of Information Science & Technology, Nanjing, China;

    Laboratory for Climate Studies, National Climate Center, CMA, Beijing, China;

    Laboratory for Climate Studies, National Climate Center, CMA, Beijing, China;

    Beijing Meteorological Bureau, CMA, Beijing, China;

    Beijing Meteorological Bureau, CMA, Beijing, China;

    Jinzhong Meteorological Bureau of Shanxi Province, CMA, Jinzhong, China;

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