深圳光合有效辐射计算方法的初探
Primary Study on Calculating Method of Photosynthetically Radiation at Shenzhen
DOI: 10.12677/AG.2018.84091, PDF,  被引量    国家自然科学基金支持
作者: 白建辉:中国科学院大气物理研究所中层大气与全球环境探测开放实验室,北京;李楠:深圳仙湖植物园,广东 深圳
关键词: 太阳辐射光合有效辐射可见光辐射吸收和散射因子Solar Radiation Photosynthetically Active Radiation Visible Radiation Cloud Absorbing and Scattering Factors
摘要: 2005年夏季在深圳对太阳辐射(包括光合有效辐射PAR、可见光辐射VIS、总辐射Q等)、气象参数等进行了综合观测,初步得到了PAR、VIS等的变化特征。观测表明,小时累计之比PAR/Q、VIS/Q、PAR/VIS相对稳定,其平均值分别为2.28 (2.61~1.88)、0.46 (0.57~0.38)、4.95 (5.23~4.47),但它们均有明显的日变化和逐日变化,并受水汽、气溶胶、云等因素的影响。建立了计算PAR、VIS的经验公式以及PAR与VIS转换关系式,计算值与观测值符合较好,PAR、VIS计算值与观测值的相对偏差分别小于3.0%、4.0%。对于经验公式在不同情况下的使用做了研究。吸收因子比散射因子对PAR、VIS的传输和计算起着更重要的作用。当同时考虑这两个因子时,可以得到实际天气较好的PAR和VIS小时累计值。
Abstract: Integrated observations were made of solar radiation (including photosynthetically active radiation (PAR), visible radiation (VIS), global radiation (Q), etc.), and meteorological parameters at Shenzhen during May 29 to June 7, 2005. The ratios of hourly sums of PAR to Q, VIS to Q and PAR to VIS were relatively stable, and their averages were 2.28 (2.61 - 1.88), 0.46 (0.57 - 0.38) and 4.95 (5.23 - 4.47), respectively. They displayed evident diurnal and daily variations and were influenced by water vapor, aerosol and clouds. Empirical models for calculating hourly sums of PAR and VIS, as well as relationship between PAR and VIS were developed. The calculated PAR and VIS were in good agreement with measured, and their relative biases were less than 3.0% and 4.0%, respectively. The applications of these empirical models under different conditions were studied. The absorbing factor plays more important role than scattering factor in atmospheric radiative transfer and calculation of PAR and visible radiation. When considering both absorbing and scattering factors, the better estimations of hourly sums of PAR and visible radiation under all sky conditions were obtained.
文章引用:白建辉, 李楠. 深圳光合有效辐射计算方法的初探[J]. 地球科学前沿, 2018, 8(4): 837-844. https://doi.org/10.12677/AG.2018.84091

参考文献

[1] 周允华, 项月琴, 栾禄凯. 光合有效通量密度的气候学计算[J]. 气象学报, 1996, 54(4): 447-455.
[2] 刘荣高, 刘纪远, 庄大方. 基于MODIS数据估算晴空陆地光合有效辐射[J]. 地理学报, 2004, 59(1): 64-73.
[3] Guenther, A., Hewitt, C.N., Erickson, D., Fall, R., Geron, C., et al. (1995) A Global Model of Natural Volatile Organic Compound Emissions. Journal of Geophysical Research: Atmospheres, 100, 8873-8892. [Google Scholar] [CrossRef
[4] 白建辉, 王明星, J. Graham, R.G. Prinn, 黄忠良. 森林排放非甲烷碳氢化合物的初步研究[J]. 大气科学, 1998, 12(2): 247-251.
[5] 季国良, 等. 张掖地区的光合有效辐射特征[J]. 高原气象, 1993, 12(2): 141-146.
[6] 田国良. 呼伦贝尔草原的太阳分光辐射能和光合潜力[J]. 地理学报, 1980, 35(1): 76-82.
[7] 谢贤群. 黄淮海平原冬小麦生育期的光合有效辐射分布特征,中国科学院“六五”黄淮海平原科技攻关文集, 黄淮海平原治理和开发, 第一集[M]. 北京: 科学出版社, 1985: 139-148.
[8] 赵名茶. 用光量子测定分析黄淮海平原冬小麦的光能利用率, 黄淮海平原治理和开发, 第一集[M]. 北京: 科学出版社, 1985: 149-161.
[9] Zhang, X.Z., Zhang, Y.G. and Zhou, Y.H. (2000) Measuring and Modeling Photosynthetically Active Radiation in Tibet Plateau during April-October. Agricultural and Forest Meteorology, 102, 207-212.
[10] Bai, J.H. (2012) Observations and Estimations of PAR and Solar Visible Radiation in North China. Journal of Atmospheric Chemistry, 69, 231-252. [Google Scholar] [CrossRef
[11] 白建辉, 王庚辰. 内蒙古草原光合有效辐射的计算方法[J]. 环境科学研究, 2004, 17(6): 15-18.
[12] 白建辉, Bradly Baker. 热带人工橡胶林异戊二烯排放通量的模式研究[J]. 环境科学学报, 2004, 24(2): 197-203.
[13] 白建辉, Brad Baker. 内蒙古草原典型草地异戊二烯的排放特征[J]. 环境科学学报, 2005, 25(3): 285-292.
[14] 黄爱葵, 李楠, A. Guenther, J. Greenberg, B. Baker, M. Graessli, 白建辉. 深圳市显著排放VOCs的园林植物调查与分析[J]. 环境科学, 2011, 32(12): 3555-3559.
[15] Bai, J.H., Duhl, T. and Hao, N. (2016) Biogenic Volatile Compound Emissions from a Temperate Forest, China: Model Simulation. Journal of Atmospheric Chemistry, 73, 29-59. [Google Scholar] [CrossRef
[16] 白建辉, 郝楠. 亚热带森林植物挥发性有机物(BVOCs)排放通量与大气甲醛之间的关系[J]. 生态环境学报, 2018, 27(6): 991-999.