Influence of changes in solar radiation on changes of surface temperature in China

Acta Meteorologica Sinica volume 27, pages87–97(2013)Cite this article

Abstract

The long-term trends of total surface solar radiation (SSR), surface diffuse radiation, and surface air temperature were analyzed in this study based on updated 48-yr data from 55 observational stations in China, and then the correlation between SSR and the diurnal temperature range (DTR) was studied. The effect of total solar radiation on surface air temperature in China was investigated on the basis of the above analyses. A strong correlation between SSR and DTR was found for the period 1961–2008 in China. The highest correlation and steepest regression line slope occurred in winter, indicating that the solar radiation effect on DTR was the largest in this season. Clouds and water vapor have strong influences on both SSR and DTR, and hence on their relationship. The largest correlations between SSR and DTR occurred in wintertime in northern China, regardless of all-day (including clear days and cloudy days) or clear-day cases.

Our results also showed that radiation arriving at the surface in China decreased significantly during 1961–1989 (dimming period), but began to increase during 1990–2008 (brightening period), in agreement with previous global studies. The reduction of total SSR offset partially the greenhouse warming during 1961–1989. However, with the increase of SSR after 1990, this offsetting effect vanished; on the contrary, it even made a contribution to the accelerated warming. Nonetheless, the greenhouse warming still played a controlling role because of the increasing of minimum and mean surface temperatures in the whole study period of 1961–2008. We estimated that the greenhouse gases alone may have caused surface temperatures to rise by 0.31–0.46°C (10 yr)−1 during 1961–2008, which is higher than previously estimated. Analysis of the corresponding changes in total solar radiation, diffuse radiation, and total cloud cover indicated that the dimming and brightening phenomena in China were likely attributable to increases in absorptive and scattering aerosols in the atmosphere, respectively.

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Author information

Affiliations

  1. Laboratory for Climate Studies, National Climate Center, China Meteorological Administration, Beijing, 100081, China

    Hua Zhang 张 华, Qing Yin 尹 青 & Peng Lu 卢 鹏

  2. Meteorological Center of Air Force in Beijing Military Area, Beijing, 100061, China

    Qing Yin 尹 青

  3. Nanjing University of Information Science & Technology, Nanjing, 210044, China

    Qing Yin 尹 青, Peng Lu 卢 鹏 & Jinhai He 何金海

  4. Center for Earth Surface System Dynamics, Atmosphere and Ocean Research Institute, University of Tokyo, Chiba, 277-8564, Japan

    Teruyuki Nakajima

  5. Kinki University, Osaka, 577-8502, Japan

    Nakata Mukai Makiko

Authors
  1. Hua Zhang 张 华
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  2. Qing Yin 尹 青
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  3. Teruyuki Nakajima
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  4. Nakata Mukai Makiko
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  5. Peng Lu 卢 鹏
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  6. Jinhai He 何金海
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Correspondence to Hua Zhang 张 华.

Additional information

Supported by the National Basic Research and Development (973) Program of China (2011CB403405), National Science and Technology Support Program of China (2008BAC40B02), and China Meteorological Adminstration Special PublicWelfare Research Fund (GYHY200906020).

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Zhang, H., Yin, Q., Nakajima, T. et al. Influence of changes in solar radiation on changes of surface temperature in China. Acta Meteorol Sin 27, 87–97 (2013). https://doi.org/10.1007/s13351-013-0109-8

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Key words

  • global dimming/brightening
  • global warming
  • surface solar radiation
  • surface air temperature