Advanced Search

WEl Wen-shouc, DONG Guang-rong. Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 839-845.
Citation: WEl Wen-shouc, DONG Guang-rong. Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 839-845.

Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example

  • Received Date: 1999-04-06
  • Publish Date: 1999-12-10
  • The radiant heat transportation at desert interface includes solar radiant heat flux,long wave radiant heat flux and desert surface heat flux. Based on the natural and climatic conditions of Gurbantunggut Desert,the author has measured and analyzed the heat budget on different underlying areas .The following results are mainly obtained: (1) The heat transportation on sand-shifting desert and on sand-fixed desert is different limited by individual surface feature,sand layer nature and air temperature etc. (2)The reflectivity and the long wave radiation on sand-shifting area are all larger than that on sand-fixed area. (3)The heat flux through sand layer increases with the layer going down;while heat transportation value changes with an inverse trend. (4)The heat transportation from earth to atmosphere on different desert types are in forms of sensible heat at daytime and latent heat at night which constitutes special response and feedback transfer process to solar radiant heat on desert area. In the meantime,the author has analyzed the changing properties of physical climate parameters in desert region according to measured data and heat balance equation of earth surface;and modeled the heat transfer process at earth-atmosphere interface.
  • [1] 1 Charney J G. Dynamics of deserts and drought in the Sahel[J].Quart. J. Roy. Meteor: Soc,1975,101:193-202

    2 Smith E A. Transition of surfaces enengy budget in Gobi desert between spring and summer season. [J] J. Climate Appl. Met,1986.25:1725-1740

    3 Henry N, Le Houerou. Climate Change,drought and desertification[J]. J Arid Environments,1996,34:133-185

    4 季国良,邹基玲.干旱地区绿洲和沙漠辐射收支的季节变化[J].高原气象,1992,13(3):323-329.

    5 魏文寿.沙漠表层粒度与水热变化的环境效应分析[J].沉积学报,1998,16(1):152-155

    6 王可丽,钟强.辐射传输模式中地表参数对大气长波辐射的影响[J].大气科学,1995,19(5):606-613

    7 魏文寿,董光荣.古尔班通古特沙漠的辐射热量交换分析[J].中国沙漠,1997, 17(4):335-341

    8 Cunnington M, Rowntree P R. Simulation of the Saharan atmosphere-dependence on moisture and albedo[J]. Quan J Roy Meteo Soc,1986, 112:971-999

    9 Kimyra F,Shimzu Y. Estunation of sensible and latent heat fluxes from soil surface temperatune using a linear air-land heat transfermodel[J]. J. App. Met.,1994,33(4):344-356

    10 Norman J R. Microclimate:The biological environment[M]. John Wiley and Sons .Second Edition,1983. 1-8

    11 何宗颖,申建友,李胜功.奈曼地区流动沙丘的地中热状况,科尔沁沙地生态环境综合整治研究[M].兰州:甘肃科学技术出版社,1993. 141-147

    12 马庆芳,方荣生,项立成等.实用热物理手册[M].北京:中国农业机械出版社,1986. 955

    13 董光荣,申建友,金炯.试论全球气候变化与沙漠的关系[J].第四纪研究,1990,1:91-98

    14 Monteith J L. Principles of environmental physics [M]. Edward Arnold .London,1973. 238-245

    15 Mabbutt J A. Desertification indicators [J]. Climate Change,1986,9:113-122

    16 Thom A S. Momentum,massed heat exchange of vegetation[J].Quart .J. Roy. Meteor .Soc .1972,98:124-134

    17 郭学良,王介民.利用简化动力学近似分析黑河实验区的感热通量[J].高原气象,1993,12(2):133-140

    18 张强.西部干旱环境同绿洲的相互作用及其与大气环流的关系,中国西部区域气候变化及其相关问题的研究[M].兰州:兰州大学出版社,1995. 50-55
  • 加载中
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(434) PDF downloads(412) Cited by()

Proportional views
Related
Publishing history
  • Received:  1999-04-06
  • Published:  1999-12-10

Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example

Abstract: The radiant heat transportation at desert interface includes solar radiant heat flux,long wave radiant heat flux and desert surface heat flux. Based on the natural and climatic conditions of Gurbantunggut Desert,the author has measured and analyzed the heat budget on different underlying areas .The following results are mainly obtained: (1) The heat transportation on sand-shifting desert and on sand-fixed desert is different limited by individual surface feature,sand layer nature and air temperature etc. (2)The reflectivity and the long wave radiation on sand-shifting area are all larger than that on sand-fixed area. (3)The heat flux through sand layer increases with the layer going down;while heat transportation value changes with an inverse trend. (4)The heat transportation from earth to atmosphere on different desert types are in forms of sensible heat at daytime and latent heat at night which constitutes special response and feedback transfer process to solar radiant heat on desert area. In the meantime,the author has analyzed the changing properties of physical climate parameters in desert region according to measured data and heat balance equation of earth surface;and modeled the heat transfer process at earth-atmosphere interface.

WEl Wen-shouc, DONG Guang-rong. Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 839-845.
Citation: WEl Wen-shouc, DONG Guang-rong. Radiant Heat Transportation at the Interface of Desert——Taking Gurbantunggut desert for example[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 839-845.
Reference (1)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return