Investigating Fire–Atmosphere Interaction in a Forest Canopy Using Wavelets

IF 2.3 3区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Ajinkya Desai, Clément Guilloteau, Warren E. Heilman, Joseph J. Charney, Nicholas S. Skowronski, Kenneth L. Clark, Michael R. Gallagher, Efi Foufoula-Georgiou, Tirtha Banerjee
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Abstract

Wildland fire–atmosphere interaction generates complex turbulence patterns, organized across multiple scales, which inform fire-spread behaviour, firebrand transport, and smoke dispersion. Here, we utilize wavelet-based techniques to explore the characteristic temporal scales associated with coherent patterns in the measured temperature and the turbulent fluxes during a prescribed wind-driven (heading) surface fire beneath a forest canopy. We use temperature and velocity measurements from tower-mounted sonic anemometers at multiple heights. Patterns in the wavelet-based energy density of the measured temperature plotted on a time–frequency plane indicate the presence of fire-modulated ramp–cliff structures in the low-to-mid-frequency band (0.01–0.33 Hz), with mean ramp durations approximately 20% shorter and ramp slopes that are an order of magnitude higher compared to no-fire conditions. We then investigate heat- and momentum-flux events near the canopy top through a cross-wavelet coherence analysis. Briefly before the fire-front arrives at the tower base, momentum-flux events are relatively suppressed and turbulent fluxes are chiefly thermally-driven near the canopy top, owing to the tilting of the flame in the direction of the wind. Fire-induced heat-flux events comprising warm updrafts and cool downdrafts are coherent down to periods of a second, whereas ambient heat-flux events operate mainly at higher periods (above 17 s). Later, when the strongest temperature fluctuations are recorded near the surface, fire-induced heat-flux events occur intermittently at shorter scales and cool sweeps start being seen for periods ranging from 8 to 35 s near the canopy top, suggesting a diminishing influence of the flame and increasing background atmospheric variability thereat. The improved understanding of the characteristic time scales associated with fire-induced turbulence features, as the fire-front evolves, will help develop more reliable fire behaviour and scalar transport models.

Abstract Image

利用小波研究林冠中火灾与大气的相互作用
野地火灾与大气层的相互作用会产生复杂的湍流模式,这种模式跨越多个尺度,为火灾蔓延行为、火苗传播和烟雾扩散提供信息。在此,我们利用基于小波的技术,探索在森林树冠下的规定风力(航向)地表火灾中,与测量温度和湍流通量的连贯模式相关的特征时间尺度。我们使用了塔式声波风速计在多个高度测量的温度和速度。在时频平面上绘制的基于小波的测量温度能量密度模式表明,在中低频段(0.01-0.33 Hz)存在火灾调制的斜坡-悬崖结构,与无火灾条件相比,平均斜坡持续时间缩短了约 20%,斜坡斜率高出一个数量级。然后,我们通过交叉小波相干性分析研究了冠层顶附近的热流和动量流事件。在火锋到达塔基之前,动量通量事件受到相对抑制,由于火焰沿风的方向倾斜,湍流通量主要由冠层顶附近的热量驱动。由暖上升气流和冷下降气流组成的火灾引起的热通量事件在一秒周期内是连贯的,而环境热通量事件主要在更高的周期(17 秒以上)运行。随后,当在地表附近记录到最强烈的温度波动时,由火焰引起的热流事件会在较短的时间尺度上间歇出现,而在树冠顶附近则开始出现 8 至 35 秒的冷扫掠,这表明火焰的影响在减弱,背景大气的变化在增加。随着火锋的演变,对与火灾诱发的湍流特征相关的特征时间尺度的进一步了解将有助于开发更可靠的火灾行为和标量传输模型。
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来源期刊
Boundary-Layer Meteorology
Boundary-Layer Meteorology 地学-气象与大气科学
CiteScore
7.50
自引率
14.00%
发文量
72
审稿时长
12 months
期刊介绍: Boundary-Layer Meteorology offers several publishing options: Research Letters, Research Articles, and Notes and Comments. The Research Letters section is designed to allow quick dissemination of new scientific findings, with an initial review period of no longer than one month. The Research Articles section offers traditional scientific papers that present results and interpretations based on substantial research studies or critical reviews of ongoing research. The Notes and Comments section comprises occasional notes and comments on specific topics with no requirement for rapid publication. Research Letters are limited in size to five journal pages, including no more than three figures, and cannot contain supplementary online material; Research Articles are generally fifteen to twenty pages in length with no more than fifteen figures; Notes and Comments are limited to ten journal pages and five figures. Authors submitting Research Letters should include within their cover letter an explanation of the need for rapid publication. More information regarding all publication formats can be found in the recent Editorial ‘Introducing Research Letters to Boundary-Layer Meteorology’.
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