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DOI | 10.1002/2016JD025506 |
Improving snow process modeling with satellite-based estimation of near-surface-air-temperature lapse rate | |
Wang, Lei; Sun, Litao; Shrestha, Maheswor; Li, Xiuping; Liu, Wenbin; Zhou, Jing; Yang, Kun; Lu, Hui; Chen, Deliang![]() | |
通讯作者 | Wang, L (通讯作者) |
发表日期 | 2016 |
ISSN | 2169-897X |
EISSN | 2169-8996 |
起始页码 | 12005 |
结束页码 | 12030 |
卷号 | 121期号:20 |
英文摘要 | In distributed hydrological modeling, surface air temperature (T-air) is of great importance in simulating cold region processes, while the near-surface-air-temperature lapse rate (NLR) is crucial to prepare T-air (when interpolating T-air from site observations to model grids). In this study, a distributed biosphere hydrological model with improved snow physics (WEB-DHM-S) was rigorously evaluated in a typical cold, large river basin (e.g., the upper Yellow River basin), given a mean monthly NLRs. Based on the validated model, we have examined the influence of the NLR on the simulated snow processes and streamflows. We found that the NLR has a large effect on the simulated streamflows, with a maximum difference of greater than 24% among the various scenarios for NLRs considered. To supplement the insufficient number of monitoring sites for near-surface-air-temperature at developing/undeveloped mountain regions, the nighttime Moderate Resolution Imaging Spectroradiometer land surface temperature is used as an alternative to derive the approximate NLR at a finer spatial scale (e.g., at different elevation bands, different land covers, different aspects, and different snow conditions). Using satellite-based estimation of NLR, the modeling of snow processes has been greatly refined. Results show that both the determination of rainfall/snowfall and the snowpack process were significantly improved, contributing to a reduced summer evapotranspiration and thus an improved streamflow simulation. |
关键词 | DISTRIBUTED HYDROLOGICAL MODELUPPER TONE RIVERPARAMETERIZATION SIB2ATMOSPHERIC GCMSUNITED-STATESRUNOFFCHINAPRODUCTSBASINVALIDATION |
英文关键词 | lapse rate; distributed hydrological model; water and energy cycle; snow process; MODIS land surface temperature |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000388293100014 |
来源期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258837 |
推荐引用方式 GB/T 7714 | Wang, Lei,Sun, Litao,Shrestha, Maheswor,et al. Improving snow process modeling with satellite-based estimation of near-surface-air-temperature lapse rate[J]. 中国科学院青藏高原研究所,2016,121(20). |
APA | Wang, Lei.,Sun, Litao.,Shrestha, Maheswor.,Li, Xiuping.,Liu, Wenbin.,...&Chen, Deliang.(2016).Improving snow process modeling with satellite-based estimation of near-surface-air-temperature lapse rate.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,121(20). |
MLA | Wang, Lei,et al."Improving snow process modeling with satellite-based estimation of near-surface-air-temperature lapse rate".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 121.20(2016). |
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