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Effect of Urbanization on Land-Surface Temperature at an Urban Climate Station in North China

机译:城市化对华北城市气候站陆地温度的影响

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While the land-surface temperature (LST) observed at meteorological stations has significantly increased over the previous few decades, it is still unclear to what extent urbanization has affected these positive trends. Based on the LST data recorded at an urban station in Shijiazhuang in North China, and two rural meteorological stations, the effect of urbanization at the Shijiazhuang station for the period 1965-2012 is examined. We find, (1) a statistically-significant linear trend in annual mean urban-rural LST difference of 0.27 degrees C (10 year)(-1), with an urbanization contribution of 100% indicating that the increase in the annual mean LST at the urban station is entirely caused by urbanization. The urbanization effects in spring, summer and autumn on the trends of mean LST are also significant; (2) the urbanization effect is small for time series of the annual mean minimum LST, and statistically marginal for the trend in annual mean maximum LST [0.19 degrees C(10 year)(-1)]; (3) the urbanization effect on the annual mean diurnal LST range (Delta LST) at the urban station is a strongly significant trend of 0.23 degrees C (10 year)(-1), with an urbanization contribution of 21%. The urbanization effects on trends in the spring and autumn mean Delta LST are also larger and more significant than for the other seasons; (4) the urbanization effects on the long-term LST trends are remarkably different from those on the near-surface air temperature at the same urban station. Nonetheless, the significant warming of the urban boundary layer is expected to affect the urban environment and ecosystems. However, the problem of data representativeness at an urban station for themonitoring and investigation of large-scale climate change remains.
机译:虽然在幽默站观察到的土地温度(LST)在前几十年中显着增加,但仍不清楚城市化影响了这些积极趋势的程度。基于在华北石家庄的城市站记录的LST数据以及两个农村气象站,研究了1965 - 2012年石家庄站的城市化对1965 - 2012年的影响。我们发现(1)年平均城乡的统计上显着的线性趋势为0.27摄氏度(10年)( - 1),城市化贡献为100%,表明年度平均值的增加城市站完全由城市化引起。春季,夏季和秋季的城市化效果对平均LST的趋势也很重要; (2)城市化效果小于年平均值最低LST的时间序列,统计上的趋势最大值最大LST [0.19摄氏度(10年)( - 1)]; (3)城市站年平均昼夜LST范围(三角洲LST)的城市化效应是0.23摄氏度(10年)( - 1)的强烈重大趋势,城市化贡献为21%。对春季和秋季趋势的城市化影响平均delta lst也比其他季节更大更大; (4)对长期LST趋势的城市化效应与同一城市站附近的近表面空气温度相同。尽管如此,预计城市边界层的显着变暖会影响城市环境和生态系统。然而,仍然存在对专题发展和调查大规模气候变化的资本站数据代表性的问题。

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