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| 青藏高原地区能量水分循环：地表能量平衡和湍流热通量 | |
| 引用本文： | 苏中波,张廷,马耀明,贾立,文军.青藏高原地区能量水分循环：地表能量平衡和湍流热通量[J].地球科学进展,2006,21(12):1224-1236. |
| 作者姓名： | 苏中波 张廷 马耀明 贾立 文军 |
| 作者单位： | 1. International Institute for Geo-Information Science and Earth Observation ITC Enschede 7500AA,the Netherlands 2. 天津市政工程局科学技术部,天津,300022 3. 中国科学院青藏高原研究所,北京,100085 4. Alterra Green World Research,Wageningen University and Research Centre Wagenigen 6700AA,the Netherlands 5. 中国科学院寒区旱区环境与工程研究所,甘肃,兰州,730000 |
| 摘 要： | 文章给出了青藏高原能量水分循环研究的概况和总结，着重估计了能量平衡各分项和湍流热通量等。在能量平衡的计算基础上，尽管能量不平衡的原因解释仍有争论并且没有解决，但我们揭示了GAME/Tibet试验观测资料中能量不平衡现象。我们发现估算的潜热通量比实际观测的要高许多。然而，根据能量平衡假设的计算结果和SEBS的估算一致性很好。在此基础上可以归纳出差异主要由GAME/Tibet试验观测资料中能量不平衡引起，潜热通量的实际观测可能偏小。 |
| 关 键 词： | 能量水分循环 青藏高原地区 能量平衡 通流通量 |
| 文章编号： | 1001-8166（2006）12-1224-13 |
| 收稿时间： | 2006-10-17 |
| 修稿时间： | 2006-10-17 |
Energy and Water Cycle over the Tibetan Plateau: Surface Energy Balance and Turbulent Heat Fluxes |
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| SU Zhong-bo,ZHANG Ting,MA Yao-ming,JIA Li,WEN Jun.Energy and Water Cycle over the Tibetan Plateau: Surface Energy Balance and Turbulent Heat Fluxes[J].Advance in Earth Sciences,2006,21(12):1224-1236. | |
| Authors: | SU Zhong-bo ZHANG Ting MA Yao-ming JIA Li WEN Jun |
| Institution: | 1.International Institute for Geo-Information Science and Earth Observation ITC Enschede 7500AA,the Netherlands; 2.Science & Technology Department, Tianjin Municipal Engineering Bureau,Tianjin 300022,China; 3.Institute of Tibetan Plateau Research, CAS, Beijing 100085,China; 4.Alterra Green World Research, Wageningen University and Research Centre Wagenigen 6700AA,the Netherlands;5.Cold and Arid Regions Environmental and Engineering Research Institute, CAS,Lanzhou 730000,China |
| Abstract: | This contribution presents an overview and an outlook of studies on energy and water cycle over the Tibetan plateau with focuses on the estimation of energy balance terms and turbulent heat fluxes. On the basis of the surface energy balance calculations, we show that the phenomena of the energy imbalance exist in GAME/Tibet experiment data, although the explanations for the reasons are debated now and not resolved yet. We found that the derived latent heat flux is much higher than the measurements. However, the corrected-measurements, which are calculated according to the hypothesis of the energy balance, compare very well with the estimation of SEBS. On this basis it is concluded that the deviation is caused by the energy imbalance of ground measurements in GAME/Tibet experiment area. The latent heat fluxes were likely under-6bserved. |
| Keywords: | Energy and water cycle The Tibetan plateau Energy balance Turbulent fluxes |
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