地球科学进展 ›› 2008, Vol. 23 ›› Issue (11): 1185 -1193. doi: 10.11867/j.issn.1001-8166.2008.11.1185

研究论文 上一篇    下一篇

地形对黄河流域太阳辐射影响的分析研究
曾燕 1,2,邱新法 3,潘敖大 2,刘昌明 4   
  1. 1.江苏省气象科学研究所,江苏 南京 210008; 2.中国科学院南京地理与湖泊研究所,江苏 南京 210008;3.南京信息工程大学遥感学院地理信息系统系,江苏 南京 210044;4.中国科学院地理科学与资源研究所,北京 100101
  • 收稿日期:2008-07-24 修回日期:2008-10-11 出版日期:2008-11-10
  • 通讯作者: 曾燕 E-mail:jlzengyan@sina.com
  • 基金资助:

    中国气象局气象新技术推广重点项目“基于DEM的我国太阳能资源评估”(编号:CMATG2006Z10)资助.

Distributed Modeling of Global Solar Radiation over Rugged Terrain of the Yellow River Basin

Zeng Yan 1,2,Qiu Xinfa 3,Pan Aoda 2,Liu Changming 4   

  1. 1.Jiangsu Institute of Meteorlogical Sciences, Nanjing 210008, China; 2.Nanjing Institute of Geography and Limnology, CAS, Nanjing 210008, China; 3.Department of GIS, School of Remote Sensing, Nanjing University of Information Science and Technology, Nanjing 210044, China;4.Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China
  • Received:2008-07-24 Revised:2008-10-11 Online:2008-11-10 Published:2008-11-10

起伏地形中太阳总辐射由直接辐射、散射辐射、周围地形反射辐射三部分组成,依据各部分太阳辐射产生机理的不同,分别设计模型以综合考虑天文因素、大气因素、宏观地理因素、局地地形因素(坡向、坡度、地形相互遮蔽)是必须的。基于数字高程模型(DEM)数据和遥感影像,在全面考虑各种因素的基础上,建立了依托常规气象站观测资料的起伏地形下太阳总辐射计算模型,完成了黄河流域1km×1km分辨率太阳总辐射分布式模拟。结果表明:受坡地自身遮蔽和周围山地相互遮蔽的影响,总体平均而言,山地接收的太阳总辐射较平地少;局地地形对太阳辐射的影响程度随季节而变,在太阳高度角较低的季节,局地地形的影响较为显著。

In rugged terrain, the global solar radiation (GSR) reaching on the surface is composed of three parts, i.e. direct solar radiation, diffuse solar radiation and terrain reflected solar radiation. The theories of these three kinds of solar radiation are different. Respective models are established which necessarily take integrated consideration of astronomical and geographic factors, local topographic factors (i.e. slope, aspect and terrain inter-shielding effect) and atmospheric physics factors are needed. Based on DEM (Digital Elevation Model) data and remote sensing data, a distributed model for calculating GSR over rugged terrain is developed, with routine meteorological observations as input. This model takes all consideration of factors influencing GSR. Using the established model, normals of annual GSR quantity with resolution of 1 km×1 km for the Yellow river basin was generated. Results suggest that influenced by local topographic factors, i.e. azimuth, slope and terrain inter-shielding effect, annual GSR quantity over mountainous areas is smaller than that over plains generally. The influences of local topographic factors on GSR are changing with seasons and are more obvious in seasons that have a lower solar elevation angle.

中图分类号: 

[1] Roberto R,Renzo R. Distributed estimation of incoming direct solar radiation over a drainage basin[J]. Journal of Hydrology,1995,166:461-478.

[2] Wong L T,Chow W K. Solar radiation model[J]. Applied Energy,2001,69:191-224.

[3] Newland F J. A study of solar radiation models for the coastal region of South China[J]. Solar Energy,1989,434:227-235.

[4] Kasten F,Czeplak G. Solar and terrestrial radiation dependent on the amount and type of cloud[J]. Solar Energy,1980,24:177-189.

[5] Davies J A,McKay D C. Evaluation of selected models for estimating solar radiation on horizontal surfaces[J]. Solar Energy,1989,433:153-168.

[6] Liu B Y H,Jordan R C. The interrelationship and characteristic distribution of direct,diffuse and total solar radiation[J]. Solar Energy,1960,4:1-19.

[7] Lam J C,Li D H W. Correlation between global solar radiation and its direct and diffuse components[J]. Building and Environment,1996,316:527-355.

[8] Bird R E,Hulstrom R L. A simplified clear-sky model for the direct and diffuse insolation on horizontal surfaces[R]. Technical Report No.SERI/TR-642-761,Golden,Colorado,CO:Solar Energy Research Institute,1981.

[9] Iqbal M. An Introduction to Solar Radiation[M]. Toronto: Academic Press,1983.

[10] Maxwell E L. METSTAT-the solar radiation model used in the production of the NSRDB[J]. Solar Energy,1998,624:263-279.

[11] Page J K. Proposed quality control procedures for the Meteorological Office data tapes relating to global solar radiation,diffuse solar radiation,sunshine and cloud in the UK[R]. Report FCIBSE,1997.

[12] Yu Guirui,He Hongli,Liu Xin′an,et al. Study on spatialization technology of terrestrial eco-information in ChinaI[J]. Journal of Natural Resources,2004,194:537-543.[于贵瑞,何洪林,刘新安,. 中国陆地生态信息空间化技术研究(——气象/气候信息的空间化技术途径[J].自然资源学报,2004,194:537-544.]

[13] He Hongli,Yu Guirui,Liu Xin′an,et al. Study on spatialization technology of terrestrial eco-information in ChinaII[J]. Journal of Natural Resources,2004,195:679-686.[何洪林,于贵瑞,刘新安,. 中国陆地生态信息空间化技术研究(——太阳辐射要素[J].自然资源学报,2004,195:679-686.]

[14] Fu Baopu. Effects of sloping fields on sunshine and solar radiation[J]. Journal of Nanjing UniversityNatural Science Edition,1958,2: 23-46.[傅抱璞. 坡地对日照和太阳辐射的影响[J]. 南京大学学报:自然科学版, 1958,2:23-46.]

[15] Fu Baopu. Mountain Climate[M]. Beijing: Science Press,1983:61-72.[傅抱璞. 山地气候[M]. 北京:科学出版社,1983:61-72.]

[16] Zhu Zhihui. The global distribution of astronomical solar radiation on nonhorizontal surfaces[J]. Science in ChinaSeries B,1988,10:1 100-1 110.[朱志辉. 非水平面天文辐射的全球分布[J]. 中国科学:B,1988,10: 1 100-1 110.]

[17] Sun Hanqun,Fu Baopu. The elliptical intergral model of computing the extraterrestrial solar radiation on the slope[J]. Acta Geographica Sinica,1996,516:559-566.[孙汉群,傅抱璞. 坡面天文辐射总量的椭圆积分模式[J]. 地理学报,1996,516:559-566.]

[18] Liu B Y,Jordan R C. Daily insulation on surfaces tilted towards the equator[J]. Transactions of the American Society of Heating,Refrigeration and Air Conditioning Engineers,1962,67:526-541.

[19] Hay J E,McKay D C. Estimating solar radiance on inclined surfaces:A review and assessment of methodologies[J]. International Journal of Solar Energy,1985,3:203-240.

[20] Dozier J,Qutcalt S I. An approach to energy balance simulation over rugged terrain[J]. Geographical Analysis,1979,11:65-85.

[21] Dozier J,Frew J. Rapid calculation of terrain parameters for radiation modeling from digital elevation data[J]. IEEE Transaction on Geoscience and Remote Sensing,1990,285:963-969.

[22] Bocquet G. Method of study and cartography of the potential sunny periods in mountainous areas[J]. Journal of Climatology, 1984,14:587-596.

[23] Stefanovic P. Insolation from digital elevation models for mountain habitat evaluation[J]. International Institute for Aerial Survey and Earth Sciences Journal,1985,3:177-186.

[24] Ranzi R,Rosso R. Distributed estimation of incoming direct solar radiation over a drainage basin[J]. Journal of Hydrology,1995,166:461-478.

[25] Li X,Cheng G D,Chen X Z,et al. Modification of solar radiation model over rugged terrain[J]. Chinese Science Bulletin,1999,4415:1 345-1 350.

[26] Li Zhanqing,Weng Duming. A computer model for calculating the duration of sunshine in mountainous areas[J]. Chinese Science Bulletin,1988,33:1 624-1 627.

[27] Zuo Dakang,Zhou Yunhua,Xiang Yueqin,et al. On Surface Radiations[M]. Beijing:Science Press,1991: 69-72.[左大康,周允华,项月琴,. 地球表层辐射研究[M]. 北京:科学出版社,1991:69-72.]

[28] Louche A,Notton G,Poggi P,et al. Correlations for direct normal and global horizontal irradiation on a French Mediterranean site[J]. Solar Energy,1991,464:261-266.

[29] Vignola F,McDaniels D K. Beam-global correlations in the Northwest Pacific[J]. Solar Energy,1986,365: 409-418.

[30] Weng Duming. Studies on Radiation Climate of China[M]. Beijing:Meteorology Press,1997:32-60.[翁笃鸣. 中国辐射气候研究[M]. 北京:气象出版社,1997:32-60.]

[31] Zeng Yan,Qiu Xinfa,Liu Changming,et al. Distributed modeling of direct solar radiation of rugged terrain over the Yellow river basin[J]. Acta Geographica Sinica,2005,485:1 028-1 033.[曾燕,邱新法,刘昌明,.起伏地形下黄河流域太阳直接辐射分布式模拟[J]. 地理学报,2005,604:680-688.]

[32] Zeng Yan,Qiu Xinfa,Liu Shaomin. Distributed modeling of extraterrestrial solar radiation over rugged terrain[J]. Chinese Journal of Geophysics,2005,485:1 028-1 033.[曾燕,邱新法,刘绍民. 起伏地形下天文辐射分布式估算模型[J].地球物理学报,2005,485:1 028-1 033.]

[33] Zeng Yan,Qiu Xinfa,Liu Changming. Distributed modeling of diffuse solar radiation over rugged terrain of the Yellow river basin[J]. Chinese Journal of Geophysics,2008,514:991-998.[曾燕,邱新法,刘昌明. 起伏地形下黄河流域太阳散射辐射分布式模拟研究[J]. 地球物理学报,2008,514:991-998.]

[34] Valiente J A,Nunez M,Lopez-Baeza E,et al. Narrow-band to broad-band conversion for Meteosat-visible channel and broad-band albedo using both AVHRR-1 and-2 channels[J]. International Journal of Remote Sensing,1995,166:1 147-1 166.

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