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Volume 22 Issue 2

Mar.  2005

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2005 >  22(2): 172-180

A Primary Study of the Variations of Vertical Radiation with the Beijing 325-m Meteorological Tower

  • 1.

    Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029


doi: 10.1007/BF02918507

  • The Beijing 325-m Meteorological Tower (325MT) is used to observe the vertical variation of solar radiation. Results of the experiments indicate that the automatic radiation monitoring system, including a sun tracker and data collection system, works well and all the specifications meet WMO observation standards. The measurement data show that there is a significant radiation decrease from 320 m to the surface, where the difference is only about 30 W m-2 on light air-pollution days, while the maximum reaches about 110 W m-2 when heavy pollution appears near the ground. The global UV radiation decreases on heavy air-pollution days and under poor visibility conditions, and the difference between 300 m and 8 m is larger than on clear days.
  • [1] Monim H.AL-JIBOORI, HU Fei, 2005: Surface Roughness Around a 325-m Meteorological Tower and Its Effect on Urban Turbulence, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 595-605.  doi: 10.1007/BF02918491
    [2] Huang Boyin, Zhao Gaoxiang, Ji Liren, 1992: A Numerical Research on the Influences of the Diurnal Variation of Solar Radiation on the Medium-Range Weather Processes, ADVANCES IN ATMOSPHERIC SCIENCES, 9, 231-236.  doi: 10.1007/BF02657513
    [3] Wang Mingxing, John W. Winchester, Lü Weixiu, Ren Lixin, Hong Zhongxiang, 1986: METEOROLOGICAL AND CHEMICAL CONTROLS ON THE VERTICAL DISTRIBUTION OF BEIJING SUMMER COARSE AND FINE AEROSOLS, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 432-442.  doi: 10.1007/BF02657933
    [4] Pratima GUPTA, Shalendra Pratap SINGH, Ashok JANGID, Ranjit KUMAR, 2017: Characterization of Black Carbon in the Ambient Air of Agra, India: Seasonal Variation and Meteorological Influence, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1082-1094.  doi: 10.1007/s00376-017-6234-z
    [5] GE Xuyang, MA Yue, ZHOU Shunwu, Tim LI, 2015: Sensitivity of the Warm Core of Tropical Cyclones to Solar Radiation, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 1038-1048.  doi: 10.1007/s00376-014-4206-0
    [6] Shunwu ZHOU, Yue MA, Xuyang GE, 2016: Impacts of the Diurnal Cycle of Solar Radiation on Spiral Rainbands, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 1085-1095.  doi: 10.1007/s00376-016-5229-5
    [7] HU Bo, WANG Yuesi, LIU Guangren, 2012: Relationship between Net Radiation and Broadband Solar Radiation in the Tibetan Plateau, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 135-143.  doi: 10.1007/s00376-011-0221-6
    [8] LI Weiping, SUN Shufen, WANG Biao, LIU Xin, 2009: Numerical Simulation of Sensitivities of Snow Melting to Spectral Composition of the Incoming Solar Radiation, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 403-412.  doi: 10.1007/s00376-009-0403-7
    [9] LIANG Hong, ZHANG Renhe, LIU Jingmiao, SUN Zhian, CHENG Xinghong, 2012: Estimation of Hourly Solar Radiation at the Surface under Cloudless Conditions on the Tibetan Plateau Using a Simple Radiation Model, ADVANCES IN ATMOSPHERIC SCIENCES, 29, 675-689.  doi: 10.1007/s00376-012-1157-1
    [10] HU Bo* and WANG Yuesi, , 2014: Variation Characteristics of Ultraviolet Radiation over the North China Plain, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 110-117.  doi: 10.1007/s00376-013-2319-5
    [11] Zou Han, Zhou Libo, Jian Yongxiao, Liu Yu, 2002: An Observational Study on the Vertical Distribution and Synoptic Variation of Ozone in the Arctic, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 855-862.  doi: 10.1007/s00376-002-0050-8
    [12] He Jinhai, Zhou Bing, Wen Min, Li Feng, 2001: Vertical Circulation Structure, lnterannual Variation Features and Variation Mechanism of Western Pacific Subtropical High, ADVANCES IN ATMOSPHERIC SCIENCES, 18, 497-510.  doi: 10.1007/s00376-001-0040-2
    [13] WEI Jiangfeng, WANG Huijun, 2004: A Possible Role of Solar Radiation and Ocean in the Mid-Holocene East Asian Monsoon Climate, ADVANCES IN ATMOSPHERIC SCIENCES, 21, 1-12.  doi: 10.1007/BF02915675
    [14] Zhao Ping, Chen Longxun, 2000: Calculation of Solar Albedo and Radiation Equilibrium over the Qinghai-Xizang Plateau and Analysis of Their Climatic Features, ADVANCES IN ATMOSPHERIC SCIENCES, 17, 140-156.  doi: 10.1007/s00376-000-0050-5
    [15] Zhaoliang ZENG, Zemin WANG, Minghu DING, Xiangdong ZHENG, Xiaoyu SUN, Wei ZHU, Kongju ZHU, Jiachun AN, Lin ZANG, Jianping GUO, Baojun ZHANG, 2021: Estimation and Long-term Trend Analysis of Surface Solar Radiation in Antarctica: A Case Study of Zhongshan Station, ADVANCES IN ATMOSPHERIC SCIENCES, 38, 1497-1509.  doi: 10.1007/s00376-021-0386-6
    [16] Yongjian HE, Zhi'an SUN, Guoping SHI, Jingmiao LIU, Jiandong LI, 2017: Modification of the SUNFLUX Solar Radiation Scheme with a New Aerosol Parameterization and Its Validation Using Observation Network Data, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1301-1315.  doi: 10.1007/s00376-016-6262-0
    [17] Hao LUO, Yong HAN, Chunsong LU, Jun YANG, Yonghua WU, 2019: Characteristics of Surface Solar Radiation under Different Air Pollution Conditions over Nanjing, China: Observation and Simulation, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 1047-1059.  doi: 10.1007/s00376-019-9010-4
    [18] Guoping SHI, Xinfa QIU, Yan ZENG, 2018: New Method for Estimating Daily Global Solar Radiation over Sloped Topography in China, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 285-295.  doi: 10.1007/s00376-017-6243-y
    [19] LIN Pengfei, LIU Hailong, ZHANG Xuehong, 2007: Sensitivity of the Upper Ocean Temperature and Circulation in the Equatorial Pacific to Solar Radiation Penetration Due to Phytoplankton, ADVANCES IN ATMOSPHERIC SCIENCES, 24, 765-780.  doi: 10.1007/s00376-007-0765-7
    [20] HU Bo, WANG Yuesi, LIU Guangren, 2008: Influences of the Clearness Index on UV Solar Radiation for Two Locations in the Tibetan Plateau---Lhasa and Haibei, ADVANCES IN ATMOSPHERIC SCIENCES, 25, 885-896.  doi: 10.1007/s00376-008-0885-8
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    • Manuscript History

    Manuscript received: 10 March 2005
    Manuscript revised: 10 March 2005
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    A Primary Study of the Variations of Vertical Radiation with the Beijing 325-m Meteorological Tower

    • 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
    • Manuscript received: 2005-03-10
    • Manuscript revised: 2005-03-10

    Abstract: The Beijing 325-m Meteorological Tower (325MT) is used to observe the vertical variation of solar radiation. Results of the experiments indicate that the automatic radiation monitoring system, including a sun tracker and data collection system, works well and all the specifications meet WMO observation standards. The measurement data show that there is a significant radiation decrease from 320 m to the surface, where the difference is only about 30 W m-2 on light air-pollution days, while the maximum reaches about 110 W m-2 when heavy pollution appears near the ground. The global UV radiation decreases on heavy air-pollution days and under poor visibility conditions, and the difference between 300 m and 8 m is larger than on clear days.

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