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Including soil water stress in process-based ecosystem models by scaling r down maximum carboxylation rate using accumulated soil water deficit

机译:在基于过程的生态系统模型中,包括使用累积的土壤水分赤字来缩放最大羧化速率,包括基于过程的生态系统模型的土壤水分胁迫

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The impacts of soil water stress on photosynthesis and stomatal conductance have not been uniformly parameterized in terrestrial ecosystem models. This study firstly quantifies diurnal variations in canopy conductance (g_(c,w)) during full-leaf periods from eddy covariance flux data at four flux sites by inverting the Penman-Monteith equation, Then, the Ball-Woodrow-Berry (BWB) slopes were derived and compared under contrasting water stress conditions by linear regression of g_(c,w) and gross primaryproductivity (GPP) derived from EC measurements. Finally, the response of the leaf maximum carboxylation rate to accumulated soil water deficit (ASWD) was explored to develop a better scheme of soil water stress. Our results show: (1) The thresholds ofrelatively available soil moisture under which soil water stress occurs were 0.575, 0.885, 0.495 and 0.653 for the tropical savanna site (AU-How), the Mediterranean forest site (IT-Col), the Mediterranean grassland site (US-Var) and the boreal forest site (CA-Oas), respectively, derived from the logistic functions of fitting g_(c,w) to relatively available soil moisture; (2) similar to previous work, we found that ensemble average g_(c,w) of dry periods were lower than those of wet periods at the studied sites, and that BWB slopes did not change significantly during droughts, indicating that BWB slopes may be conserved under prolonged drought; and (3) EC-derived GPP gradually decreased with the increase of ASWD, which can be well captured by a V_(mr)-ASWD scheme developed in this study. In sum, the V_(mr)-ASWD scheme would increase the accuracy of GPP simulations of ecosystem models. This study suggests that the change of BWB slopes under prolonged drought is not justified according to the experimental data examined while adjusting V_(cmax) with ASWD accounts for the change in leaf physiology due to prolonged drought and is computationally feasible and efficient.
机译:土壤水分胁迫对光合作用和气孔传导的影响并未在地面生态系统模型中均匀参数化。本研究首先通过将Penman-Monteith方程逆转到四个助焊位方形的涡流传感器磁通数据的全叶期间,在四个助焊场的全叶期间定量遮盖孔电导(G_(C,W))的昼夜变化。通过基于EC测量的G_(C,W)和源自EC测量的总初级产品(GPP)对比水胁迫条件下衍生并比较斜坡。最后,探讨了叶片最大羧化率与累积土壤水赤字(ASWD)的响应,以发展更好的土壤水分胁迫方案。我们的结果表明:(1)热带大草原网站(Au-How),地中海森林网站(IT-COL),地中海(IT-COL),地中海(IT-COL),地中海森林网站(IT-COL),地中海(Au-Col)的阈值为0.575,0.885,0.495和0.653,为0.575,0.885,0.495和0.653草地网站(US-VAR)和北方森林网站(CA-OAS)分别来自拟合G_(C,W)的逻辑功能,以相对可获得的土壤水分; (2)与以前的工作类似,我们发现干燥时期的集合平均G_(C,W)低于研究部位的湿时期,并且在干旱期间BWB斜率没有显着变化,表明BWB斜坡可能在长期干旱下保守; (3)EC衍生的GPP随着ASWD的增加逐渐减少,这可以通过本研究中开发的V_(MR)-ASWD方案进行很好的捕获。总之,V_(MR)-ASWD方案将提高生态系统模型GPP模拟的准确性。本研究表明,根据在调整V_(CMAX)的实验数据,随着ASWD占叶片生理学的变化而在调整v_(cmax)的同时,对延长干旱的BWB斜率的变化并非有合理的。

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