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[中国青藏高原植被水分利用效率的时空变化及其与气候因子的关系]

[Spatial-temporal variation of vegetation water use efficiency and its relationship with climate factors over the Qinghai-Tibet Plateau, China].

作者信息

Cui Xi-Lin, He Yun-Ling, Li Zong-Shan

机构信息

School of Earth Sciences, Yunnan University, Kunming 650500, China.

Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2022 Jun;33(6):1525-1532. doi: 10.13287/j.1001-9332.202206.024.

Abstract

Water use efficiency (WUE) is an effective index to study the coupling of land carbon and water cycle. The Qinghai-Tibet Plateau is the most important ecological security barrier in China. Understanding the characteristics and mechanism of WUE is important for the carbon cycle and water resources rational utilization in the plateau. Based on MODIS data of gross primary productivity (GPP) and evapotranspiration (ET), we analyzed the spatial-temporal variations of WUE over the Qinghai-Tibet Plateau and the effects of climate factors. The results showed that WUE in the Qinghai-Tibet Plateau had an upward trend under the combined action of GPP and ET during 2001-2020. The southeast and northeast of the Plateau had the highest WUE value, while the central part had the lowest WUE value. WUE of grassland, marsh and alpine vegetation showed an increasing trend, while that of shrub land, broadleaved forest and coniferous forest showed a decreasing trend. There was a significant positive correlation between WUE and annual air temperature, and the sensitivity increased with the increases of air temperature. The relationship between WUE and annual precipitation was non-linear. When precipitation was less than 700 mm, the sensitivity of WUE to precipitation decreased with the increases of precipitation. When precipitation was more than 700 mm, the sensitivity of precipitation increased with the increases of precipitation. However, WUE was negatively correlated with precipitation in more than 75% of regions, and was affected by precipitation in a larger area. In the future, warm and humid climate would lead to a decrease in WUE.

摘要

水分利用效率(WUE)是研究陆地碳循环与水循环耦合关系的有效指标。青藏高原是中国最重要的生态安全屏障。了解水分利用效率的特征及机制对高原地区的碳循环和水资源合理利用具有重要意义。基于MODIS的总初级生产力(GPP)和蒸散量(ET)数据,我们分析了青藏高原水分利用效率的时空变化及气候因子的影响。结果表明,2001—2020年期间,在GPP和ET的共同作用下,青藏高原的水分利用效率呈上升趋势。高原东南部和东北部的水分利用效率值最高,而中部地区的水分利用效率值最低。草地、沼泽和高山植被的水分利用效率呈上升趋势,而灌木林、阔叶林和针叶林的水分利用效率呈下降趋势。水分利用效率与年气温之间存在显著正相关,且随着气温升高敏感性增强。水分利用效率与年降水量之间呈非线性关系。当降水量小于700毫米时,水分利用效率对降水的敏感性随降水量增加而降低。当降水量大于700毫米时,降水敏感性随降水量增加而增加。然而,在超过75%的区域,水分利用效率与降水量呈负相关,且受降水影响的区域面积较大。未来,温暖湿润的气候将导致水分利用效率降低。

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