Development of an enthalpy-based frozen soil model and its validation in a cold region in China
文献类型：期刊论文
| 作者 | Koike, T (Koike, Toshio)1; Bao, HY (Bao, Huiyi)1; Yang, K (Yang, Kun)2,3; Bao, HY; Lawford, P (Lawford, Peter)1; Shrestha, M (Shrestha, Maheswor)4; Wang, L (Wang, Lei)2,3 |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
 |
| 出版日期 | 2016 |
| 卷号 | 121期号:10页码:5259-5280 |
| 关键词 | Distributed Hydrological Model Simultaneous Heat Climate-change Permafrost Region Water Model Parameterization Temperature Simulation Plateau Scheme |
| DOI | 10.1002/2015JD024451 |
| 文献子类 | Article |
| 英文摘要 | An enthalpy-based frozen soil model was developed for the simulation of water and energy transfer in cold regions. To simulate the soil freezing/thawing processes stably and efficiently, a three-step algorithm was applied to solve the nonlinear governing equations: (1) a thermal diffusion equation was implemented to simulate the heat conduction between soil layers; (2) a freezing/thawing scheme used a critical temperature criterion to judge the phase status and introduced enthalpy and total water mass into freezing depression equation to represent ice formation/melt and corresponding latent heat release/absorption; and (3) a water flow scheme was employed to describe the liquid movement within frozen soil. In addition, a parameterization set of hydraulic and thermal properties was updated by considering the frozen soil effect. The performance of the frozen soil model was validated at point scale in a typical mountainous permafrost basin of China. An ice profile initialization method is proposed for permafrost modeling. Results show that the model can achieve a convergent solution at a time step of hourly and a surface layer thickness of centimeters that are typically used in current land surface models. The simulated profiles of soil temperature, liquid water content, ice content and thawing front depth are in good agreement with the observations and the characteristics of permafrost. The model is capable of continuously reproducing the diurnal and seasonal freeze-thaw cycle and simulating frozen soil hydrological processes. |
| 学科主题 | 自然地理学 |
| 语种 | 英语 |
| WOS记录号 | WOS:000381629900009 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/7695]  |
| 专题 | 青藏高原研究所_图书馆 |
| 通讯作者 | Bao, HY |
| 作者单位 | 1.Univ Tokyo, Dept Civil Engn, Tokyo, Japan 2.Chinese Acad Sci, Lab Tibetan Environm Changes & Land Surface Proc, Inst Tibetan Plateau Res, Beijing, Peoples R China 3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 4.Water & Energy Commiss Secretariat, Water Resources Div, Kathmandu, Nepal |
| 推荐引用方式 GB/T 7714 | Koike, T ,Bao, HY ,Yang, K ,et al. Development of an enthalpy-based frozen soil model and its validation in a cold region in China[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2016,121(10):5259-5280. |
| APA | Koike, T .,Bao, HY .,Yang, K .,Bao, HY.,Lawford, P .,...&Wang, L .(2016).Development of an enthalpy-based frozen soil model and its validation in a cold region in China.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,121(10),5259-5280. |
| MLA | Koike, T ,et al."Development of an enthalpy-based frozen soil model and its validation in a cold region in China".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 121.10(2016):5259-5280. |
入库方式： OAI收割
来源：青藏高原研究所
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