Assessment of Noah land surface model with various runoff parameterizations over a Tibetan river | |
Zheng, Donghai1; Van der Velde, Rogier1; Su, Zhongbo1; Wen, Jun2; Wang, Xin2 | |
刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES |
2017-02-16 | |
卷号 | 122期号:3页码:1488-1504 |
ISSN号 | 2169-897X |
DOI | 10.1002/2016JD025572 |
通讯作者 | Zheng, Donghai(d.zheng@utwente.nl) |
英文摘要 | Runoff parameterizations currently adopted by the (i) NoahMP model, (ii) Community Land Model (CLM), and (iii) CLM with variable infiltration capacity hydrology (CLMVIC) are incorporated into the structure of Noah land surface model, and the impact of these parameterizations on the runoff simulations is investigated for a Tibetan river. Four numerical experiments are conducted with the default Noah and three aforementioned runoff parameterizations. Each experiment is forced with the same set of atmospheric forcing, vegetation, and soil parameters. In addition, the Community Earth System Model database provides the maximum surface saturated area parameter for the NoahMP and CLM parameterizations. A singleyear recurrent spinup is adopted for the initialization of each model run to achieve equilibrium states. Comparison with discharge measurements shows that each runoff parameterization produces significant differences in the separation of total runoff into surface and subsurface components and that the soil water storagebased parameterizations (Noah and CLMVIC) outperform the groundwater tablebased parameterizations (NoahMP and CLM) for the seasonally frozen and highaltitude Tibetan river. A parameter sensitivity experiment illustrates that this underperformance of the groundwater tablebased parameterizations cannot be resolved through calibration. Further analyses demonstrate that the simulations of other surface water and energy budget components are insensitive to the selected runoff parameterizations, due to the strong control of the atmosphere on simulated land surface fluxes induced by the diurnal dependence of the roughness length for heat transfer and the large water retention capacity of the highly organic top soils over the plateau. |
收录类别 | SCI |
WOS关键词 | SOIL-MOISTURE ; CLIMATE-CHANGE ; HEAT FLUXES ; PLATEAU ; SIMULATION ; IMPACTS ; PHYSICS ; AUGMENTATIONS ; PRECIPITATION ; TEMPERATURE |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
出版者 | AMER GEOPHYSICAL UNION |
WOS记录号 | WOS:000396119200007 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2558003 |
专题 | 寒区旱区环境与工程研究所 |
通讯作者 | Zheng, Donghai |
作者单位 | 1.Univ Twente, Fac Geoinformat Sci & Earth Observat, Enschede, Netherlands 2.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold A, Lanzhou, Peoples R China |
推荐引用方式 GB/T 7714 | Zheng, Donghai,Van der Velde, Rogier,Su, Zhongbo,et al. Assessment of Noah land surface model with various runoff parameterizations over a Tibetan river[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(3):1488-1504. |
APA | Zheng, Donghai,Van der Velde, Rogier,Su, Zhongbo,Wen, Jun,&Wang, Xin.(2017).Assessment of Noah land surface model with various runoff parameterizations over a Tibetan river.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(3),1488-1504. |
MLA | Zheng, Donghai,et al."Assessment of Noah land surface model with various runoff parameterizations over a Tibetan river".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.3(2017):1488-1504. |
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