Journal of Geographical Sciences, Volume. 30, Issue 9, 1387(2020)

Spatio-temporal variation in China’s climatic seasons from 1951 to 2017

Bin MA1, Bo ZHANG1、*, and Lige JIA1,2
Author Affiliations
  • 1College of Geography and Environmental Science, Northwest Normal University, Lanzhou 730070, China
  • 2Tourism College, Inner Mongolia Normal University, Huhhot 010022, China
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    Figures & Tables(11)
    Location of the meteorological stations. R is the goodness of fit between missing data and completion data in China
    Spatial distribution of climatic seasonal regions in different Climate Normals in China
    Spatial distribution of spring, summer, autumn and winter duration in different Climate Normals in China
    Linear trends and cumulative anomaly curves in different climatic seasonal regions from 1951 to 2017
    Spatial distribution of expanded area for climatic seasonal regions in China after 1994
    Trends of spring, summer, autumn and winter durations from 1951 to 2017
    Trends of the spring, summer, autumn and winter starting dates in China from 1951 to 2017
    • Table 1.

      Threshold temperatures for different climatic seasons

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      Table 1.

      Threshold temperatures for different climatic seasons

      SeasonsSpringSummerAutumnWinter
      Threshold$10\ \le T{{\overline{M}}_{j}}<22\ $℃$T{{\overline{M}}_{j}}\ge 22\ $℃$10\ \le T{{\overline{M}}_{j}}<22\ $℃$T{{\overline{M}}_{j}}<10\ $℃
    • Table 2.

      Definition of normal climatic seasonal regions

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      Table 2.

      Definition of normal climatic seasonal regions

      Climatic seasons regionsAbbreviationThreshold for the temperature of tenderness
      Perennial-winter regionPWR$T{{\overline{M}}_{j}}<10$℃
      Perennial-summer regionPSuR$T{{\overline{M}}_{j}}\ge 22$℃
      Perennial-spring regionPSpR$10\le T{{\overline{M}}_{j}}<22$℃
      No-winter regionNWR$T{{\overline{M}}_{j}}\ge 10$℃
      No-summer regionNSR$T{{\overline{M}}_{j}}<22$℃
      Discernible regionDRExcept the above five cases
    • Table 3.

      Multiple regression models for climatic seasonal length simulation in China for different Climate Normals

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      Table 3.

      Multiple regression models for climatic seasonal length simulation in China for different Climate Normals

      Climate NormalThresholdMultiple regression modelR2Significance level
      1951-198010 ℃$\begin{align} & Y=4014.82\text{+}41.71\times \theta \text{+}0.003\times {{\theta }^{3}}-4.32\times \text{sin}\theta -1280.2\times \\ & \ \ \ \ \ \ \text{ln}\theta -119.38\times \text{ln}\varphi -0.02\times h \\ \end{align}$0.970.001
      22 ℃$\begin{align} & Y=3461.58+93.51\times \theta -0.65\times {{\theta }^{2}}\text{+}2.42\times \text{sin}\theta -1759.02\times \\ & \ \ \ \ \ \ \text{ln}\theta -121.4\times \text{ln}\varphi -0.09\times h \\ \end{align}$0.9580.001
      1961-199010 ℃$\begin{align} & Y=4025.87\text{+}41.94\times \theta -0.003\times {{\theta }^{3}}-4.28\times \text{sin}\theta -1285.43\times \\ & \ \ \ \ \ \ \text{ln}\theta -119.33\times \text{ln}\varphi -0.02\times h \\ \end{align}$0.970.001
      22 ℃$\begin{align} & Y=3461.57\text{+}93.51\times \theta -0.65\times {{\theta }^{2}}\text{+}2.42\times \text{sin}\theta -1759.02\times \\ & \ \ \ \ \ \ \text{ln}\theta -121.4\times \text{ln}\varphi -0.09\times h \\ \end{align}$0.9580.001
      1971-200010 ℃$\begin{align} & Y=4009.6\text{+}41.7\times \theta -0.003\times {{\theta }^{3}}-5.39\times \text{sin}\theta -1280.05\times \\ & \ \ \ \ \ \ \text{ln}\theta -118.44\times \text{ln}\varphi -0.02\times h \\ \end{align}$0.970.001
      22 ℃$\begin{align} & Y=3682.63\text{+}105.4\times \theta -0.74\times {{\theta }^{2}}\text{+}1.75\times \text{sin}\theta -1964.13\times \\ & \ \ \ \ \ \ \text{ln}\theta -165.82\times \text{ln}\varphi -0.1\times h \\ \end{align}$0.9580.001
      1981-201010 ℃$\begin{align} & Y=3801.72\text{+}38.03\times \theta -0.003\times {{\theta }^{3}}-5.44\times \text{sin}\theta -1193.74\times \\ & \ \ \ \ \ \ \text{ln}\theta -114.2\times \text{ln}\varphi -0.02\times h \\ \end{align}$0.970.001
      22 ℃$\begin{align} & Y=3395.83\text{+}67.93\times \theta -0.006\times {{\theta }^{3}}\text{+}2.1\times \text{sin}\theta -1671.14\times \\ & \ \ \ \ \ \ \text{ln}\theta -147\times \text{ln}\varphi -0.1\times h \\ \end{align}$0.9590.001
    • Table 4.

      The R, S and RMSE between measured and simulated values of the validation site

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      Table 4.

      The R, S and RMSE between measured and simulated values of the validation site

      StationRSRSMEStationRSRSME
      Hailar0.9961.215.05Dardo0.9979.3322.77
      Karamay0.9847.8723.47Yanyuan0.99109.7617.15
      Korla0.9956.0819.86Zhanyi0.99124.6524.16
      Yarkant0.9962.225.61Gaoping0.9977.554.40
      Naomaohu0.9844.7917.10Shuangfeng0.9963.334.76
      Jiuquan0.9972.0315.55Xuzhou0.9957.503.45
      Gonghe0.9961.2010.06Anqing0.9962.443.26
      Urad Zhongqi0.9968.656.08Wenzhou0.9977.666.83
      Houma0.9958.183.94Du’an0.9988.153.00
      Changchun0.9956.584.68Meixian0.9987.596.98
      Qinglong0.9960.404.03Tainan0.9976.5948.13
      Sog0.9835.708.39Qionghai0.9960.2416.26
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    Bin MA, Bo ZHANG, Lige JIA. Spatio-temporal variation in China’s climatic seasons from 1951 to 2017[J]. Journal of Geographical Sciences, 2020, 30(9): 1387

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    Paper Information

    Category: Research Articles

    Received: Dec. 17, 2019

    Accepted: Jun. 2, 2020

    Published Online: Apr. 21, 2021

    The Author Email: Bo ZHANG (zhangbo@nwnu.edu.cn)

    DOI:10.1007/s11442-020-1788-6

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