Toledo Naomi, Moulatlet Gabriel, Gaona Gabriel, Valencia Bryan, Hirata Ricardo, Conicelli Bruno
Facultad de Ciencias de la Tierra y Agua, Universidad Regional Amazónica Ikiam, Tena 150150, Ecuador.
Arizona Institute for Resilience, University of Arizona, Tucson, USA; Department of Ecology and Evolutionary Biology, University of Arizona, Tucson, USA.
Sci Total Environ. 2024 Dec 1;954:176612. doi: 10.1016/j.scitotenv.2024.176612. Epub 2024 Oct 1.
Over recent decades, anthropogenic forest fires have significantly altered vegetation dynamics in the Amazon region. While human activities primarily initiate these fires, their escalation is intricately linked to climatic conditions, particularly droughts induced by the warm El Niño phase. This study investigates the impact of meteorological and hydrological drought on forest fires in the Amazon, focusing on the role of groundwater and El Niño events. Utilizing comprehensive drought indicators at various soil depths and standardized precipitation indexes, the research spans from 2004 to 2016, revealing a consistent decrease in humidity conditions across surface soil moisture, root zone soil moisture, and groundwater storage levels. With its slower response to precipitation changes, groundwater emerges as a crucial factor influencing hydrological drought patterns in the Amazon. The spatial distribution of drought conditions is explored, highlighting areas with lower humidity concentrations in the northeast and a correlation between forest fires and positive rates of change in burned area fraction during El Niño events. Notably, the study underscores the substantial increase in burned area during the 2015-2016, characterized by a very strong El Niño. This nuanced understanding of groundwater dynamics and its interplay with El Niño events provides critical insights for developing a tailored fire risk index in the ecologically significant and vulnerable Amazon basin, subsidizing strategies for mitigating fire risk and enhancing preparedness.
在最近几十年里,人为引发的森林火灾显著改变了亚马逊地区的植被动态。虽然人类活动是这些火灾的主要引发因素,但其火势升级与气候条件密切相关,特别是与温暖的厄尔尼诺阶段引发的干旱有关。本研究调查了气象干旱和水文干旱对亚马逊地区森林火灾的影响,重点关注地下水和厄尔尼诺事件的作用。利用不同土壤深度的综合干旱指标和标准化降水指数,该研究涵盖了2004年至2016年,结果显示地表土壤湿度、根区土壤湿度和地下水位储存水平的湿度条件持续下降。由于地下水对降水变化的响应较慢,它成为影响亚马逊地区水文干旱模式的关键因素。研究探讨了干旱条件的空间分布,突出了东北部湿度浓度较低的地区,以及厄尔尼诺事件期间森林火灾与燃烧面积比例变化率为正之间的相关性。值得注意的是,该研究强调了2015 - 2016年期间燃烧面积的大幅增加,这一时期的特点是出现了非常强烈的厄尔尼诺现象。这种对地下水动态及其与厄尔尼诺事件相互作用的细致理解,为在生态意义重大且脆弱的亚马逊流域制定量身定制的火灾风险指数、补贴减轻火灾风险和加强防范的策略提供了关键见解。