中国农业气象

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栾城地区光合有效辐射的测量与计算*

白建辉;   

  1. 中国科学院大气物理研究所中层大气和全球环境探测重点实验室;
  • 出版日期:2010-04-10 发布日期:2010-04-10
  • 基金资助:
    中国科学院野外台站研究基金项目

Measurement and Calculation of Photosynthetically Active Radiation at Luancheng Region

BAI Jian-hui(Key Laboratory of Middle Atmosphere and Globe Environment Observation,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China)   

  • Online:2010-04-10 Published:2010-04-10

摘要: 2005年7月19日-2006年9月30日,在河北栾城对太阳辐射包括光合有效辐射QPAR、可见光辐射QVIS、总辐射Q等气象参数开展了4次综合观测,初步得到了QPAR、QVIS等的变化特征。观测表明,小时累计之比QPAR/Q、QVIS/Q、QPAR/QVIS相对稳定,其平均值分别为1.94mol.MJ-1、0.39、4.95mol.MJ-1,同时它们均表现出明显的日、逐日、季节变化特征,并受到水汽、气溶胶、云等因素的影响。建立了计算实际天气QPAR、QVIS小时累计的经验公式及QPAR与QVIS转换关系式,计算值与观测值均吻合较好。在考虑水汽和散射因子时,QPAR、QVIS计算值与观测值的相对偏差分别为14.4%、13.9%;限于资料缺乏,也可仅考虑水汽因子的作用,此时QPAR、QVIS的相对偏差分别为15.2%、14.2%。利用比值法计算QPAR、QVIS时,水汽因子具有重要作用,气溶胶因子的作用远弱于水汽因子,但仍需要考虑。

关键词: 太阳辐射, 光合有效辐射, 可见光辐射, 云, 水汽, 散射因子

Abstract: Integrated measurement on the solar radiation (including photosynthetically active radiation (QPAR),visible radiation (QVIS),global radiation (Q),and etc.),meteorological parameters at Luancheng were made four times during July 19,2005 to September 31,2006. The variation characteristics of QPAR and QVIS were obtained. The results showed that the ratios of hourly sum of QPAR to Q,QVIS to Q,QPAR to QVIS were relatively stable,averaging at 1.94 mol MJ-1,0.39,4.95 mol MJ-1,respectively. These ratios displayed obvious diurnal,daily and seasonal variations,and were influenced by water vapor,aerosol,clouds and etc. The empirical formulas were built up for calculating hourly sums of QPAR and QVIS and their relationship under actual sky conditions. The calculated QPAR and QVIS were in accordance with the observed data,and their relative biases were 14.4% and 13.9%,respectively,when water vapor and scattering factor were considered. In the actual condition with only water vapor factor considered,their relative biases were 15.2% and 14.2%,respectively. Water vapor played a very important role for the estimation of hourly sums of QPAR and QVIS by using the ratio of QPAR/Q,QVIS/Q. Aerosol's role is less important,but it should also be considered.

Key words: Solar radiation, Solar radiation, Photosynthetically active radiation, Visible radiation, Cloud, Water vapor, Scattering factor