The impacts of net long-wave radiation on the surface soil thermal regimes over the Qinghai–Tibetan Plateau, China

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• 作者：Ren Li ; Lin Zhao ; Tonghua Wu ; Xiaodong Wu ; Yao Xiao…
• 关键词：Net long ; wave radiation ; Soil thermal regime ; Freezing–thawing intensity ; Qinghai–Tibetan Plateau
• 刊名：Environmental Earth Sciences
• 出版年：2016
• 出版时间：February 2016
• 年：2016
• 卷：75
• 期：3
• 全文大小：846 KB
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• 作者单位：Ren Li (1)
  Lin Zhao (1)
  Tonghua Wu (1)
  Xiaodong Wu (1)
  Yao Xiao (1)
  Yizhen Du (1)
  Yanhui Qin (1)
  
  1. Cryosphere Research Station on the Qinghai-Tibet Plateau, State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, China
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：None Assigned
• 出版者：Springer Berlin Heidelberg
• ISSN：1866-6299

文摘

Radiation data measured at six stations on the Qinghai–Tibetan Plateau (QTP) were used to analyze the variation of net long-wave radiation (L _n ). The stations were located in the arid, semiarid, and sub-humid climate zones, covering the major climate types of the QTP. The impacts of L _n , combined with soil temperature data, on the thermal regime of ground surfaces were evaluated. L _n varied regionally over the QTP. It decreased in the northeastern and western parts and the interior of the QTP, while it showed an increasing trend in the southeastern part of the QTP. L _n declined significantly at a rate of 0.415 MJ m−2 day−1 per decade during the past 20 years. L _n greatly influenced the freezing index (DDF). DDF and the surface freezing–thawing intensity (FTI) increased with decreasing L _n . L _n was negatively correlated with FTI and this was most pronounced with a 2-year-lag FTI. The ratio of L _n /R _s (R _s denotes the global radiation) was greater than the surface albedo (R _k /R _s ) (R _k denotes the reflected radiation). Both parameters resulted in surface energy loss and a lowering of the surface temperature. The cooling effect of L _n /R _s exceeds that of R _k /R _s .