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退化对亚马逊热带森林水、能量和碳循环的影响。

Impacts of Degradation on Water, Energy, and Carbon Cycling of the Amazon Tropical Forests.

作者信息

Longo Marcos, Saatchi Sassan, Keller Michael, Bowman Kevin, Ferraz António, Moorcroft Paul R, Morton Douglas C, Bonal Damien, Brando Paulo, Burban Benoît, Derroire Géraldine, Dos-Santos Maiza N, Meyer Victoria, Saleska Scott, Trumbore Susan, Vincent Grégoire

机构信息

Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA.

Institute of Environment and Sustainability University of California Los Angeles CA USA.

出版信息

J Geophys Res Biogeosci. 2020 Aug;125(8):e2020JG005677. doi: 10.1029/2020JG005677. Epub 2020 Aug 20.

DOI:10.1029/2020JG005677
PMID:32999796
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7507752/
Abstract

Selective logging, fragmentation, and understory fires directly degrade forest structure and composition. However, studies addressing the effects of forest degradation on carbon, water, and energy cycles are scarce. Here, we integrate field observations and high-resolution remote sensing from airborne lidar to provide realistic initial conditions to the Ecosystem Demography Model (ED-2.2) and investigate how disturbances from forest degradation affect gross primary production (GPP), evapotranspiration (ET), and sensible heat flux (H). We used forest structural information retrieved from airborne lidar samples (13,500 ha) and calibrated with 817 inventory plots (0.25 ha) across precipitation and degradation gradients in the eastern Amazon as initial conditions to ED-2.2 model. Our results show that the magnitude and seasonality of fluxes were modulated by changes in forest structure caused by degradation. During the dry season and under typical conditions, severely degraded forests (biomass loss ≥66%) experienced water stress with declines in ET (up to 34%) and GPP (up to 35%) and increases of H (up to 43%) and daily mean ground temperatures (up to 6.5°C) relative to intact forests. In contrast, the relative impact of forest degradation on energy, water, and carbon cycles markedly diminishes under extreme, multiyear droughts, as a consequence of severe stress experienced by intact forests. Our results highlight that the water and energy cycles in the Amazon are driven by not only climate and deforestation but also the past disturbance and changes of forest structure from degradation, suggesting a much broader influence of human land use activities on the tropical ecosystems.

摘要

选择性采伐、森林破碎化以及林下火灾直接破坏了森林结构和组成。然而,关于森林退化对碳、水和能量循环影响的研究却很匮乏。在此,我们整合了实地观测数据和机载激光雷达的高分辨率遥感数据,为生态系统人口统计学模型(ED - 2.2)提供现实的初始条件,并研究森林退化带来的干扰如何影响总初级生产力(GPP)、蒸散量(ET)和感热通量(H)。我们利用从机载激光雷达样本(13500公顷)中获取并通过横跨亚马逊东部降水和退化梯度的817个清查样地(0.25公顷)校准得到的森林结构信息,作为ED - 2.2模型的初始条件。我们的结果表明,通量的大小和季节性受到退化引起的森林结构变化的调节。在旱季和典型条件下,与未受破坏的森林相比,严重退化的森林(生物量损失≥66%)经历了水分胁迫,ET下降(高达34%),GPP下降(高达35%),H增加(高达43%),日平均地面温度升高(高达6.5°C)。相比之下,在极端的多年干旱期间,由于未受破坏的森林也经历了严重胁迫,森林退化对能量、水和碳循环的相对影响显著减小。我们的结果突出表明,亚马逊地区的水和能量循环不仅受气候和森林砍伐驱动,还受过去的干扰以及森林退化导致的结构变化影响,这表明人类土地利用活动对热带生态系统的影响更为广泛。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/c6a96c98c51e/JGRG-125-e2020JG005677-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/0fbf20da2371/JGRG-125-e2020JG005677-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/b31e57cdcb53/JGRG-125-e2020JG005677-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/88a0021226cd/JGRG-125-e2020JG005677-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/dd9c61213139/JGRG-125-e2020JG005677-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/0a96942853c3/JGRG-125-e2020JG005677-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/83b705040ee3/JGRG-125-e2020JG005677-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/e23cf06d31d6/JGRG-125-e2020JG005677-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/c9669036c942/JGRG-125-e2020JG005677-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/c6a96c98c51e/JGRG-125-e2020JG005677-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/0fbf20da2371/JGRG-125-e2020JG005677-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/b31e57cdcb53/JGRG-125-e2020JG005677-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/88a0021226cd/JGRG-125-e2020JG005677-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/dd9c61213139/JGRG-125-e2020JG005677-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/0a96942853c3/JGRG-125-e2020JG005677-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/83b705040ee3/JGRG-125-e2020JG005677-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/e23cf06d31d6/JGRG-125-e2020JG005677-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/c9669036c942/JGRG-125-e2020JG005677-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/93fc/7507752/c6a96c98c51e/JGRG-125-e2020JG005677-g009.jpg

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