Gora Evan M, McGregor Ian R, Muller-Landau Helene C, Burchfield Jeffrey C, Cushman K C, Rubio Vanessa E, Mori Gisele Biem, Sullivan Martin J P, Chmielewski Matthew W, Esquivel-Muelbert Adriane
Cary Institute of Ecosystem Studies, New York, New York, USA.
Smithsonian Tropical Research Institute, Balboa, Republic of Panama.
Ecol Lett. 2025 Jul;28(7):e70157. doi: 10.1111/ele.70157.
Tropical forest dynamics and composition have changed over recent decades, but the proximate drivers of these changes remain unclear. Investigations into these trends have focused on increasing drought stress, CO, temperature, and fires, whereas convective storms are generally overlooked. We argue that existing literature provides clear support for the importance of storms as drivers of forest change. We reanalyze the largest plot-based study of tropical forest carbon dynamics to show that lightning frequency-an indicator of storm activity-strongly predicts forest carbon storage and residence time, and its inclusion improves model fit and weakens evidence for the effects of high temperatures. Convective storm activity has increased 5%-25% per decade over the past half century. Extrapolating from historic trends, we estimate that storms likely contribute ca. 50% of the reported increases in biomass mortality across Amazonia, with all realistic combinations of assumptions indicating a possible range of 12%-118%. Spatial variation in storm activity shows weak relationships with drought, demonstrating that forests can experience high drought stress, high storm activity, or both. Accordingly, we hypothesise that convective storms are among the most important drivers of tropical forest change, and as such, they require significant research investment to avoid misguiding science, policy, and management.
近几十年来,热带森林的动态和组成发生了变化,但这些变化的直接驱动因素仍不明确。对这些趋势的调查主要集中在干旱压力增加、二氧化碳、温度和火灾上,而对流风暴通常被忽视。我们认为,现有文献明确支持风暴作为森林变化驱动因素的重要性。我们重新分析了最大规模的基于样地的热带森林碳动态研究,以表明闪电频率(风暴活动的一个指标)能有力地预测森林碳储存和停留时间,将其纳入模型可改善模型拟合,并削弱高温影响的证据。在过去半个世纪里,对流风暴活动每十年增加5% - 25%。根据历史趋势推断,我们估计风暴可能占亚马逊地区报告的生物量死亡率增加的约50%,所有合理的假设组合表明可能范围为12% - 118%。风暴活动的空间变化与干旱的关系较弱,这表明森林可能经历高干旱压力、高风暴活动,或两者皆有。因此,我们假设对流风暴是热带森林变化的最重要驱动因素之一,正因如此,需要大量研究投入,以避免误导科学、政策和管理。