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2
Drought sensitivity of the Amazon rainforest.亚马逊雨林的干旱敏感性。
Science. 2009 Mar 6;323(5919):1344-7. doi: 10.1126/science.1164033.
3
Increasing risk of Amazonian drought due to decreasing aerosol pollution.气溶胶污染减少导致亚马逊地区干旱风险增加。
Nature. 2008 May 8;453(7192):212-5. doi: 10.1038/nature06960.
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Impact of a drier Early-Mid-Holocene climate upon Amazonian forests.全新世早中期气候变干对亚马孙森林的影响。
Philos Trans R Soc Lond B Biol Sci. 2008 May 27;363(1498):1829-38. doi: 10.1098/rstb.2007.0019.
5
Effects of large-scale Amazon forest degradation on climate and air quality through fluxes of carbon dioxide, water, energy, mineral dust and isoprene.大规模亚马逊森林退化通过二氧化碳、水、能量、矿物粉尘和异戊二烯通量对气候和空气质量的影响。
Philos Trans R Soc Lond B Biol Sci. 2008 May 27;363(1498):1873-80. doi: 10.1098/rstb.2007.0027.
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Towards quantifying uncertainty in predictions of Amazon 'dieback'.迈向量化亚马逊“森林枯死”预测中的不确定性。
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亚马逊地区气候和植被指数的季节性和年际变化。

Seasonal and interannual variability of climate and vegetation indices across the Amazon.

机构信息

Instituto de Pesquisa Ambiental da Amazônia, 66035-170 Belém, Brazil.

出版信息

Proc Natl Acad Sci U S A. 2010 Aug 17;107(33):14685-90. doi: 10.1073/pnas.0908741107. Epub 2010 Aug 2.

DOI:10.1073/pnas.0908741107
PMID:20679201
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC2930478/
Abstract

Drought exerts a strong influence on tropical forest metabolism, carbon stocks, and ultimately the flux of carbon to the atmosphere. Satellite-based studies have suggested that Amazon forests green up during droughts because of increased sunlight, whereas field studies have reported increased tree mortality during severe droughts. In an effort to reconcile these apparently conflicting findings, we conducted an analysis of climate data, field measurements, and improved satellite-based measures of forest photosynthetic activity. Wet-season precipitation and plant-available water (PAW) decreased over the Amazon Basin from 1996-2005, and photosynthetically active radiation (PAR) and air dryness (expressed as vapor pressure deficit, VPD) increased from 2002-2005. Using improved enhanced vegetation index (EVI) measurements (2000-2008), we show that gross primary productivity (expressed as EVI) declined with VPD and PAW in regions of sparse canopy cover across a wide range of environments for each year of the study. In densely forested areas, no climatic variable adequately explained the Basin-wide interannual variability of EVI. Based on a site-specific study, we show that monthly EVI was relatively insensitive to leaf area index (LAI) but correlated positively with leaf flushing and PAR measured in the field. These findings suggest that production of new leaves, even when unaccompanied by associated changes in LAI, could play an important role in Basin-wide interannual EVI variability. Because EVI variability was greatest in regions of lower PAW, we hypothesize that drought could increase EVI by synchronizing leaf flushing via its effects on leaf bud development.

摘要

干旱对热带森林的新陈代谢、碳储量,最终对碳向大气的通量都有强烈的影响。基于卫星的研究表明,亚马逊森林在干旱期间会变绿,因为光照增加,而实地研究则报告称,在严重干旱期间,树木死亡率增加。为了调和这些明显相互矛盾的发现,我们分析了气候数据、实地测量和改进的基于卫星的森林光合作用活动测量。1996 年至 2005 年期间,亚马逊盆地的雨季降水和植物可用水(PAW)减少,而光合有效辐射(PAR)和空气干燥度(以蒸气压亏缺 VPD 表示)从 2002 年至 2005 年增加。使用改进的增强植被指数(EVI)测量值(2000 年至 2008 年),我们表明,在研究的每一年,在广泛的环境中,在稀疏树冠覆盖的区域,总初级生产力(以 EVI 表示)随着 VPD 和 PAW 的增加而下降。在森林茂密的地区,没有任何气候变量能够充分解释整个盆地的 EVI 年际变化。基于一项特定地点的研究,我们表明,每月的 EVI 相对不敏感于叶面积指数(LAI),但与实地测量的叶发芽和 PAR 呈正相关。这些发现表明,即使没有相关的 LAI 变化,新叶的产生也可能在整个盆地的 EVI 年际变化中发挥重要作用。由于 EVI 变化在 PAW 较低的地区最大,我们假设干旱可能通过其对叶芽发育的影响来同步叶发芽,从而增加 EVI。