Evaluation of three complementary relationship approaches for evapotranspiration over the Yellow River basin | |
Liu S. M. ; Sun R. ; Sun Z. P. ; Li X. O. ; Liu C. M. | |
2006 | |
关键词 | evapotranspiration complementary relationship modelling spatial distribution Yellow River basin regional evapotranspiration areal evapotranspiration nonsaturated surfaces potential evaporation taylor parameter heat-flux model transpiration priestley layer |
英文摘要 | Regional evapotranspiration is an important component of the hydrological cycle. However. reliable estimates of regional evapotranspiration are extremely difficult to obtain. In this study, the evapotranspiration simulated by three complementary relationship approaches, namely the Advection-Aridity (AA) model, the Complementary Relationship Areal Evapotranspiration (CRAE) model and the Granger (G) model. is evaluated With the observations over the Yellow River basin during 1981-2000. The simulations on overall annual evapotranspiration are reasonably good. with mean annual errors less than 10% except in extreme dry Years. The AA model gives the best estimation for the monthly evapotranspiration, and the CRAE and GM models slightly overestimate in winter. In addition, the AA model presents the same closure error of water balance over the Yellow River basin as model G. which was less than that by the CRAE model. In rather dry and rather wet cases (with higher or lower available energy). all three models perform less well. Empirical parameters of these models need to be recalibrated before they can be applied to other regions. The distribution of evapotranspiration over the Yellow River basin is also discussed. Copyright (c) 2006 John Wiley & Sons, Ltd. |
出处 | Hydrological Processes |
卷 | 20 |
期 | 11 |
页 | 2347-2361 |
收录类别 | SCI |
语种 | 英语 |
ISSN号 | 0885-6087 |
内容类型 | SCI/SSCI论文 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/23437] ![]() |
专题 | 地理科学与资源研究所_历年回溯文献 |
推荐引用方式 GB/T 7714 | Liu S. M.,Sun R.,Sun Z. P.,et al. Evaluation of three complementary relationship approaches for evapotranspiration over the Yellow River basin. 2006. |
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