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Structural Uncertainty in Model-Simulated Trends of Global Gross Primary Production

机译:全球初级生产总值的模型模拟趋势中的结构不确定性

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Projected changes in the frequency and severity of droughts as a result of increase in greenhouse gases have a significant impact on the role of vegetation in regulating the global carbon cycle. Drought effect on vegetation Gross Primary Production (GPP) is usually modeled as a function of Vapor Pressure Deficit (VPD) and/or soil moisture. Climate projections suggest a strong likelihood of increasing trend in VPD, while regional changes in precipitation are less certain. This difference in projections between VPD and precipitation can cause considerable discrepancies in the predictions of vegetation behavior depending on how ecosystem models represent the drought effect. In this study, we scrutinized the model responses to drought using the 30-year record of Global Inventory Modeling and Mapping Studies (GIMMS) 3g Normalized Difference Vegetation Index (NDVI) dataset. A diagnostic ecosystem model, Terrestrial Observation and Prediction System (TOPS), was used to estimate global GPP from 1982 to 2009 under nine different experimental simulations. The control run of global GPP increased until 2000, but stayed constant after 2000. Among the simulations with single climate constraint (temperature, VPD, rainfall and solar radiation), only the VPD-driven simulation showed a decrease in 2000s, while the other scenarios simulated an increase in GPP. The diverging responses in 2000s can be attributed to the difference in the representation of the impact of water stress on vegetation in models, i.e., using VPD and/or precipitation. Spatial map of trend in simulated GPP using GIMMS 3g data is consistent with the GPP driven by soil moisture than the GPP driven by VPD, confirming the need for a soil moisture constraint in modeling global GPP.
机译:温室气体增加导致的干旱频率和严重程度的预计变化将对植被在调节全球碳循环中的作用产生重大影响。通常将干旱对植被总初级生产力(GPP)的影响建模为蒸气压赤字(VPD)和/或土壤湿度的函数。气候预测表明VPD上升趋势的可能性很大,而降水的区域变化则不确定。 VPD和降水之间的这种预测差异可能会导致植被行为的预测存在相当大的差异,具体取决于生态系统模型如何表示干旱效应。在这项研究中,我们使用了30年的全球清单建模和制图研究(GIMMS)3g归一化差异植被指数(NDVI)数据集来审查模型对干旱的反应。一种诊断生态系统模型,即地面观测和预测系统(TOPS),用于在9种不同的实验模拟下估算1982年至2009年的全球GPP。全球GPP的控制运行一直持续到2000年,但在2000年之后保持不变。在具有单一气候约束(温度,VPD,降雨和太阳辐射)的模拟中,只有VPD驱动的模拟在2000年代有所下降,而其他情况模拟了GPP的增长。在2000年代,不同的响应可以归因于模型中使用水分胁迫和/或降水所代表的水分胁迫对植被影响的差异。在使用GIMMS 3g数据的模拟GPP中,趋势的空间图与由土壤水分驱动的GPP与由VPD驱动的GPP一致,这证实了在对全局GPP建模时需要土壤水分约束。

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