F. de Sales, Zackary Werner, João Gilberto de Souza Ribeiro
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引用次数: 0
Abstract
This study uses a combined research approach based on remote-sensing and numerical modeling to quantify the effects of burned areas on the surface climate in the two Brazilian biomes most affected by fires: the tropical savanna and the Amazon rainforest. Our estimates indicate that between 2007 and 2020, approximately 6% of the savanna and 2% of the rainforest were burned on average. Non-parametric regressions based on 14-year climate model simulations indicate that latent heat flux decreases on average by approximately 0.17 W m−2 in the savanna and 0.60 W m−2 in the rainforest per each 1 km2 burned, with most of the impacts registered during the onset of the wet season. Sensible and ground heat fluxes are also impacted but at less intensity. Surface air is also warmer and drier, especially over rainforest burned sites. On average, fire reduced gross primary production in the savanna and rainforest by 12% and 10%, respectively, in our experiments.
本研究采用基于遥感和数值模拟的综合研究方法,量化了受火灾影响最严重的两个巴西生物群落:热带稀树草原和亚马逊雨林的燃烧面积对地表气候的影响。我们的估计表明,在2007年至2020年间,平均约有6%的热带草原和2%的雨林被烧毁。基于14年气候模式模拟的非参数回归表明,每燃烧1 km2,热带草原的潜热通量平均减少约0.17 W m−2,雨林的潜热通量平均减少0.60 W m−2,其中大部分影响记录在雨季开始期间。感热通量和地热通量也受到影响,但强度较小。地表空气也变得更加温暖和干燥,尤其是在雨林被烧毁的地方。在我们的实验中,火灾平均使热带稀树草原和雨林的总初级生产分别减少了12%和10%。