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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.
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    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

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    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
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  • 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.
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