Optimization of canopy resistance models for alpine meadow in the northeastern Tibetan Plateau
Optimization of canopy resistance models for alpine meadow in the northeastern Tibetan Plateau
复制标题
青藏高原东北部高寒草甸冠层抗性模型优化
DOI:
10.1016/j.jhydrol.2022.128007
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发表时间:
2022-06
影响因子:
6.4
通讯作者:
Shiqiang Zhang
中科院分区:
文献类型:
--
作者:
Yaping Chang;Yongjian Ding;Qiudong Zhao;Jia Qin;Shiqiang Zhang
• Twelve combination models of the Jarvis-type model were compared for canopy resistance estimation of alpine meadows. • Six-year eddy covariance data were used to evaluate the model performance. • The model 10 (M10) performed best for the alpine meadow. • Selection of appropriate stress functions is essential for canopy resistance modeling. Canopy resistance ( r c ) is a critical parameter for estimating vegetation transpiration. The site-specific r c can be calculated using the inversed Penman-Monteith (PM) equation with the effective leaf area index (LAI), which requires meteorological and turbulent flux data. The spatial distribution of r c is difficult to characterize due to the harsh environment of the Tibetan Plateau. The Jarvis-type model for modeling r c , described as a multiplicative function of environmental variables, has been widely used. However, the differences and optimization of different Jarvis-type models for alpine meadows have not been fully addressed. Consequently, our overall objective was to determine the appropriate functions for r c estimation and improve its accuracy for the alpine meadow ecosystem. Twelve Jarvis-type models composed of different stress functions were examined and compared with the observed r c calculated using PM equation at the Arou site in the northeastern Tibetan Plateau. The results suggest that the proper air temperature function and vapor pressure deficit function could improve model performance obviously. There was no obvious difference between the two different stress functions of downward shortwave radiation. The best model (M10), which was composed of an asymptotical function of downward shortwave radiation, a linear function of air temperature, an exponential function of vapor pressure deficit and a piecewise function of soil water content, had best performance with coefficient of determination of 0.93, root mean square error of 60.2 s m −1 and Nash-Sutcliffe efficiency coefficient of 0.92. The selection of proper stress functions is important for r c modeling. Models that considered the air temperature for r c calculations produced better results than those without temperature. The sensitivity analysis of r c to environmental variables indicated that r c was most sensitive to vapor pressure deficit, followed by LAI and downward shortwave radiation, whereas r c was less sensitive to soil water content. For all optimized parameters, r c was the most sensitive to k T (a fitting parameter for temperature), followed by k D (a fitting parameter for vapor pressure deficit) and r cmin (minimum r c under the optimal physiological condition). This study addresses the selection of proper stress functions in modeling r c for the alpine meadow site, which can also provide a reference for other ecosystems.
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影响因子:
6.2
作者:
Xu Shiqin;Yu Zhongbo;Zhang Ke;Ji Xibin;Yang Chuanguo;Sudicky Edward A.
通讯作者:
Sudicky Edward A.
影响因子:
6.2
作者:
Sha Zhou;Bofu Yu;Yao Zhang;Yuefei Huang;Guangqian Wang
通讯作者:
Sha Zhou;Bofu Yu;Yao Zhang;Yuefei Huang;Guangqian Wang
DOI:
10.1175/1520-0450(2001)040
发表时间:
2001-08
期刊:
Journal of Applied Meteorology
影响因子:
--
作者:
E. Valor;V. Meneu;V. Caselles
通讯作者:
E. Valor;V. Meneu;V. Caselles
影响因子:
3.2
作者:
T. Yabe;R. Tanaka;T. Nakamura;F. Xiao
通讯作者:
T. Yabe;R. Tanaka;T. Nakamura;F. Xiao
DOI:
10.1071/pp98023
发表时间:
1999
期刊:
Australian Journal of Plant Physiology
影响因子:
--
作者:
D. White;C. Beadle;P. Sands;D. Worledge;J. Honeysett
通讯作者:
D. White;C. Beadle;P. Sands;D. Worledge;J. Honeysett