Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site

The surface fluxes calculated in land surface models (LSMs) are sensitive to the determination of the stability parameter. Further, calculation of the surface fluxes over the Tibetan Plateau (TP) is crucial in the simulation of regional and global weather and climate. In this study, we use 2-year mi...

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Main Authors: Xingbing Zhao, Zhiwei Heng, Xingwen Jiang, Qidong Yang, Yubin Li, Yuanjian Yang, Zhiqiu Gao
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Land
Subjects:
Online Access:https://www.mdpi.com/2073-445X/10/3/253
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author Xingbing Zhao
Zhiwei Heng
Xingwen Jiang
Qidong Yang
Yubin Li
Yuanjian Yang
Zhiqiu Gao
author_facet Xingbing Zhao
Zhiwei Heng
Xingwen Jiang
Qidong Yang
Yubin Li
Yuanjian Yang
Zhiqiu Gao
author_sort Xingbing Zhao
collection DOAJ
description The surface fluxes calculated in land surface models (LSMs) are sensitive to the determination of the stability parameter. Further, calculation of the surface fluxes over the Tibetan Plateau (TP) is crucial in the simulation of regional and global weather and climate. In this study, we use 2-year micrometeorological data measured from Shiquanhe, located in the western TP, to evaluate the performance of the widely used Noah LSM with five stability parameterization schemes. Results show that all five stability parameterization schemes can generally reproduce the observations, but the scheme proposed by Li has the smallest bias. The reason is that Li’s scheme is more accurate under the unstable condition, and the surface layer at Shiquanhe is mostly unstable. Further, the four non-iterative schemes show an advantage in terms of their computational efficiency compared to the iterative scheme adopted by the Noah LSM.
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spelling doaj.art-8adc9465134f4656860bb6e364af96b62023-12-03T12:16:21ZengMDPI AGLand2073-445X2021-03-0110325310.3390/land10030253Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan SiteXingbing Zhao0Zhiwei Heng1Xingwen Jiang2Qidong Yang3Yubin Li4Yuanjian Yang5Zhiqiu Gao6School of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaInstitute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, ChinaInstitute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, ChinaDepartment of Atmospheric Science, Yunnan University, Kunming 650091, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaSchool of Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing 210044, ChinaThe surface fluxes calculated in land surface models (LSMs) are sensitive to the determination of the stability parameter. Further, calculation of the surface fluxes over the Tibetan Plateau (TP) is crucial in the simulation of regional and global weather and climate. In this study, we use 2-year micrometeorological data measured from Shiquanhe, located in the western TP, to evaluate the performance of the widely used Noah LSM with five stability parameterization schemes. Results show that all five stability parameterization schemes can generally reproduce the observations, but the scheme proposed by Li has the smallest bias. The reason is that Li’s scheme is more accurate under the unstable condition, and the surface layer at Shiquanhe is mostly unstable. Further, the four non-iterative schemes show an advantage in terms of their computational efficiency compared to the iterative scheme adopted by the Noah LSM.https://www.mdpi.com/2073-445X/10/3/253land surface modelthe Tibetan Plateaustability parameternon-iterative scheme
spellingShingle Xingbing Zhao
Zhiwei Heng
Xingwen Jiang
Qidong Yang
Yubin Li
Yuanjian Yang
Zhiqiu Gao
Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
Land
land surface model
the Tibetan Plateau
stability parameter
non-iterative scheme
title Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
title_full Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
title_fullStr Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
title_full_unstemmed Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
title_short Evaluation of the Effect of Stability Schemes on the Simulation of Land Surface Processes at a Western Tibetan Site
title_sort evaluation of the effect of stability schemes on the simulation of land surface processes at a western tibetan site
topic land surface model
the Tibetan Plateau
stability parameter
non-iterative scheme
url https://www.mdpi.com/2073-445X/10/3/253
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