期刊文献+

三江平原地区光合有效辐射观测研究 被引量:4

Observational Study of Variation of Photosynthetically Active Radiation in the Sanjiang Plain
下载PDF
导出
摘要 利用2005~2011年的太阳辐射观测资料分析三江平原地区光合有效辐射(Qp)的时间变化特征及其与总辐射(Rs)比值(Qp/Rs)的变化规律,结果表明,Qp与Rs具有相同的季节变化特征;Qp日累计值的变化范围为60.47~0.11 mol m^-2 d^-1,年均值为23.76 mol m^-2 d^-1。Qp/Rs的变化范围为1.52~2.07 mol MJ^-1,年均值为1.91 mol MJ^-1。Qp/Rs和Qp季节变化一致,两者都是夏季最大,春秋次之,冬季最小。通过利用2011年的Qp观测数据、大气质量数与晴空指数的相互关系,建立了适合于估量三江地区 Qp的经验方程,估算值与观测值的相对误差在5.7%以内。 The variation of photosynthetically active radiation (Qp) and ratio of Qp to broadband solar radiation (Rs) at Sanjiang in Northeast China were analyzed on the basis of in situ data measured during 2005-2011. The results indicate that the seasonal and diurnal variation of Qp are similar to those of Rs. The daily values of Qp range from 0.11 to 60.47 mol m^-2, with an average annual value of 23.76 mol m^-2. The daily values of Qp/Rs range from 1.52-2.07 mol MJ^-1, with an average annual value of 1.91 mol MJ-1. The seasonal variation of Qp/Rs is similar to that of Qp. Qp and Qp/Rs reach a maximum in summer and a minimum in winter. An estimation equation for Qp was established on the basis of the optical air mass, clearness index, and Qp data measured in 2011. Evaluation of the results shows that this estimation equation can be used to calculate historical Qp data with a relative error within 5.7%.
作者 胡波 王跃思
出处 《气候与环境研究》 CSCD 北大核心 2014年第3期343-350,共8页 Climatic and Environmental Research
基金 国家自然科学基金41275165 41021004
关键词 光合有效辐射 估算方程 三江平原 Photosynthetically Active Radiation Estimation equation Sanjiang Plain
  • 相关文献

参考文献21

  • 1Alados I, Foyo-Moreno I, Alados-Arboledas L. 1996. Photosynthetically active radiation: Measurements and modelling [J]. Agricultural and Forest Meteorology, 78 (1-2): 121-131. 被引量:1
  • 2Britton C M, Dodd J D. 1976. Relationships of photosynthetic active radiation and shortwave irradiation [J]. Agricultural and Forest Meteorology, 17: 1-17. 被引量:1
  • 3Dye D G. 2004. Spectral composition and quanta-to-energy ratio of diffuse photosynthetically active radiation under diverse cloud conditions [J]. J. Geophys. Res., 109, dio:10.1029/2003JD004251. 被引量:1
  • 4Elhadidy M A, Abdel-Nabi D Y, Kruss P D. 1990. Ultraviolet solar radiation at Dhahran, Saudi Arabia [J]. Solar Energy, 44 (6): 315-319. 被引量:1
  • 5Foyo-Moreno I, Vida J, Alados-arboledas L. 1999. A simple all weather model to estimate ultraviolet solar radiation (290-385 nm) [J]. J. Appl. Meteor., 38 (7): 1020-1026. 被引量:1
  • 6Geger M, Diabaté L, Ménard L, et al. 2002. A web service for controlling the quality of measurements of global solar irradiation [J]. Solar Energy, 73 (6): 475-480. 被引量:1
  • 7Gueymard C. 1989. A two-band model for the calculation of clear sky solar irradiance, illuminance, and photosynthetically active radiation at the earth's surface [J]. Solar Energy, 43 (5): 253-265. 被引量:1
  • 8Gueymard C A. 2004. The Sun's total and spectral irradiance for solar energy applications and solar radiation models [J]. Solar Energy, 76: 423-453. 被引量:1
  • 9Hu B, Wang Y S, Liu G R. 2010. Long-term trends in photosynthetically active radiation in Beijing [J]. Advances in Atmospheric Sciences, 27 (6): 1380-1388. 被引量:1
  • 10胡波,王跃思,刘广仁.太阳紫外/光合有效辐射表标定方法探讨[J].气候与环境研究,2010,15(2):210-216. 被引量:4

二级参考文献55

共引文献43

同被引文献47

引证文献4

二级引证文献12

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部