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Seasonally and spatially varied controls of climatic factors on net primary productivity in alpine grasslands on the Tibetan Plateau

机译:青藏高原高寒草原气候因素对净初级生产力的季节性和空间变化控制

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摘要

Vegetation net primary productivity (NPP) is a core parameter regulating carbon cycles of terrestrial ecosystem, which also has close relations with climates. The alpine ecosystems on the Tibetan Plateau (TP) are highly sensitive to climate changes. However, systematic analyses on the seasonal and annual responses of NPP to climatic factors in different grassland types on the TP are still lacking. In this study, the spatial and temporal patterns of NPP and their responses to temperature, precipitation and solar radiation during 2001–2015?at seasonal and annual temporal scales were investigated based on outputs of an improved Carnegie–Ames–Stanford Approach (CASA) model. The improved CASA model showed solid performances in simulating NPP in reference to field observations ( R sup2/sup?=?0.79, P ??0.001), resulting in mean error (ME) of ?16.68, root mean square error (RMSE) of 87.59?g?C·msup?2/sup·yrsup?1/sup, and mean relative error (MRE) of ?4.29%, respectively. The annual NPP displayed different altitude dependences between the regions below and above 3500?m, which could be attributed to the altitude associated precipitation variations. The temporal trends of the seasonal and annual NPP exhibited high spatial heterogeneity. For the entire alpine grasslands, solar radiation exerted stronger influences on annual NPP than temperature and precipitation did. The responses of NPP to climatic factors also varied among grassland types and seasons. For alpine meadow, solar radiation and temperature were the dominant climatic factors in controlling the NPP variability in spring and summer, respectively, while the effect of precipitation was weak in all seasons. On the contrary, precipitation played a more crucial role in influencing NPP than temperature and solar radiation in both summer and autumn for alpine steppe. Our results shed further lights on the mechanism underlying the responses of alpine ecosystem to climate changes. The improved understanding can provide guidelines for alpine grassland management.
机译:植被净初级生产力(NPP)是调节陆地生态系统碳循环的核心参数,它也与气候密切相关。青藏高原(TP)的高山生态系统对气候变化高度敏感。但是,仍然缺乏对黄土高原不同类型草地上NPP对气候因子的季节和年度响应的系统分析。在这项研究中,基于改进的卡内基-艾姆斯-斯坦福方法(CASA)模型的输出,研究了2001-2015年NPP的时空分布及其对季节,年度时间尺度上温度,降水和太阳辐射的响应。 。改进的CASA模型显示了参考现场观测结果模拟NPP的可靠性能(R 2 ?=?0.79,P 0.001),导致平均误差(ME)为16.68,均方根平方误差(RMSE)为87.59?g?C·m ?2 ·yr ?1 ,平均相对误差(MRE)为4.29%。年度NPP在3500μm以下和以上的区域之间显示出不同的海拔依赖性,这可以归因于海拔相关的降水变化。季节性和年度NPP的时间趋势显示出高度的空间异质性。对于整个高山草原,太阳辐射对年NPP的影响要比温度和降水影响更大。在草原类型和季节之间,NPP对气候因素的响应也有所不同。对于高寒草甸来说,太阳辐射和温度是控制春季和夏季NPP变异的主要气候因素,而降水在所有季节均较弱。相反,对于高山草原而言,降水在影响NPP方面比夏季和秋季的温度和太阳辐射更重要。我们的研究结果进一步揭示了高山生态系统对气候变化的响应机制。增进了解可以为高山草原管理提供指导。

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