Increased Occurrence of Large-Scale Windthrows Across the Amazon Basin

IF 8.3 Q1 GEOSCIENCES, MULTIDISCIPLINARY AGU Advances Pub Date : 2024-11-01 DOI:10.1029/2023AV001030
J. David Urquiza-Muñoz, Susan Trumbore, Robinson I. Negrón-Juárez, Yanlei Feng, Alexander Brenning, C. Michael Vasquez-Parana, Daniel Magnabosco Marra
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Abstract

Convective storms with strong downdrafts create windthrows: snapped and uprooted trees that locally alter the structure, composition, and carbon balance of forests. Comparing Landsat imagery from subsequent years, we documented temporal and spatial variation in the occurrence of large (≥30 ha) windthrows across the Amazon basin from 1985 to 2020. Over 33 individual years, we detected 3179 large windthrows. Windthrow density was greatest in the central and western Amazon regions, with ∼33% of all events occurring in ∼3% of the monitored area. Return intervals for large windthrows in the same location of these “hotspot” regions are centuries to millennia, while over the rest of the Amazon they are >10,000 years. Our data demonstrate a nearly 4-fold increase in windthrow number and affected area between 1985 (78 windthrows and 6,900 ha) and 2020 (264 events and 32,170 ha), with more events of >500 ha size since 1990. Such extremely large events (>500 ha up to 2,543 ha) are responsible for interannual variation in the overall median (84 ± 5.2 ha; ±95% CI) and mean (147 ± 13 ha) windthrow area, but we did not find significant temporal trends in the size distribution of windthrows with time. Our results document increased damage from convective storms over the past 40 years in the Amazon, filling a gap in temporal records for tropical regions. Our publicly accessible large windthrow database provides a valuable tool for exploring dynamic conditions leading to damaging storms and their ecological impact on Amazon forests.

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亚马逊流域大规模风蚀现象增多
具有强下沉气流的对流风暴会产生风倒树:折断和连根拔起的树木会局部改变森林的结构、组成和碳平衡。通过比较随后几年的陆地卫星图像,我们记录了1985年至2020年亚马逊流域大面积(≥30公顷)风障发生的时间和空间变化。在 33 个年份中,我们发现了 3179 次大型风拔。亚马逊中部和西部地区的风崩密度最大,33%的风崩事件发生在3%的监测区域内。在这些 "热点 "地区的同一地点,大风抛的回归间隔为几个世纪到上千年,而在亚马逊河的其他地区,回归间隔为 1 万年。我们的数据显示,1985 年(78 次风灾,6,900 公顷)至 2020 年(264 次风灾,32,170 公顷)期间,风灾次数和受影响面积增加了近 4 倍,自 1990 年以来,500 公顷规模的风灾次数更多。这些超大型事件(>500公顷至2,543公顷)是造成总体中位数(84 ± 5.2公顷;±95% CI)和平均值(147 ± 13公顷)风箭面积年际变化的原因,但我们没有发现风箭面积分布随时间变化的显著时间趋势。我们的研究结果表明,在过去的 40 年中,亚马逊地区对流风暴造成的破坏不断增加,填补了热带地区时间记录的空白。我们可公开访问的大型风卷草数据库为探索导致破坏性风暴的动态条件及其对亚马逊森林的生态影响提供了宝贵的工具。
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