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Mechanistic Processes Controlling Persistent Changes of Forest Canopy Structure After 2005 Amazon Drought

机译:2005年亚马逊干旱后控制森林冠层结构持续变化的机械过程

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The long-term impact of Amazonian drought on canopy structure has been observed in ground and remote sensing measurements. However, it is still unclear whether it is caused by biotic (e.g., plant structure damage) or environmental (e.g., water deficiency) factors. We used the Community Land Model version 4.5 (CLM4.5) and radar backscatter observations from SeaWinds Scatterometer on board QuikSCAT (QSCAT) satellite to investigate the relative role of biotic and environmental factors in controlling the forest canopy disturbance and recovery processes after the 2005 Amazonian drought. We validated the CLM4.5 simulation of the drought impact and the recovery of leaf carbon (C) pool, an indicator of canopy structure, over southwestern Amazonia with QSCAT backscatter observations, which are sensitive to canopy structure change. We found that the leaf C pool simulated by CLM4.5 recovered to the 2000-2009 mean level (343 g C m~(-2)) in 3 years after a sharp decrease in 2005, consistent with the QSCAT observed slow recovery.Through sensitivity experiments, we found that the slow C recovery was primarily due to biotic factors represented by the canopy damage and reduction of plant C pools. The recovery of soil water and the coupling between water and C pools, which is an environmental factor, only contributes ~24% to the leaf C recovery. The results showed (1) the strength of scatterometer backscatter measurements in capturing canopy damage over tropical forests and in validating C cycle models and (2) the biotic factors play the dominant role in regulating the drought induced disturbance and persistent canopy changes in CLM4.5.
机译:在地面和遥感测量中观察到Amazonian干旱对冠层结构的长期影响。然而,目前尚不清楚它是由生物(例如,植物结构损伤)或环境(例如,水缺乏)因素引起的。我们使用社区土地模型4.5版(CLM4.5)和雷达反向散射观察,从Quikscat(QSCAT)卫星上的Seawinds散射仪进行了反向散射观察,以调查生物和环境因素在2005年亚马逊的森林树冠扰动和恢复过程中的相对作用干旱。我们经过验证了对干旱影响的CLM4.5模拟和叶碳(C)池的恢复,在亚马逊西南部的亚马丘西亚冠层结构的指标,具有QSCAT反向散射观察,这对冠层结构变化敏感。我们发现,2005年3年后,CLM4.5模拟的叶C池恢复到2000-2009平均水平(343克C m〜(-2)),与QScat观察到缓慢恢复的QSCAT一致。敏感性实验,我们发现缓慢的C恢复主要是由于冠层损伤所代表的生物因子和植物C池的减少。土壤水和水和C池之间的耦合回收,即环境因素,仅​​贡献叶片C恢复〜24%。结果表明(1)散射仪反向散射测量的强度在热带森林上捕获冠层损伤以及验证C循环模型和(2)生物因素在调节干旱诱导的CLM4.5中发挥着主导作用。 。

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