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利用小波研究森林冠层中的火灾-大气相互作用

Investigating Fire-Atmosphere Interaction in a Forest Canopy Using Wavelets.

作者信息

Desai Ajinkya, Guilloteau Clément, Heilman Warren E, Charney Joseph J, Skowronski Nicholas S, Clark Kenneth L, Gallagher Michael R, Foufoula-Georgiou Efi, Banerjee Tirtha

机构信息

Department of Civil and Environmental Engineering, University of California, Irvine, CA 92697 USA.

Northern Research Station, USDA Forest Service, Lansing, MI 48910 USA.

出版信息

Boundary Layer Meteorol. 2024;190(5):21. doi: 10.1007/s10546-024-00862-0. Epub 2024 Apr 18.

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.

摘要

野火与大气的相互作用会产生复杂的湍流模式,这些模式在多个尺度上组织起来,影响着火势蔓延行为、火旋风传输和烟雾扩散。在此,我们利用基于小波的技术,探索在森林冠层下规定的风驱动(顺风)地表火期间,与测量温度和湍流通量中的相干模式相关的特征时间尺度。我们使用安装在塔上的超声风速仪在多个高度测量温度和速度。在时频平面上绘制的测量温度的基于小波的能量密度模式表明,在低频到中频带(0.01 - 0.33赫兹)存在火灾调制的斜坡 - 悬崖结构,与无火条件相比,平均斜坡持续时间约短20%,斜坡斜率高一个数量级。然后,我们通过交叉小波相干分析研究冠层顶部附近的热通量和动量通量事件。在火前沿到达塔基之前不久,由于火焰在风向的倾斜,动量通量事件相对受到抑制,冠层顶部附近的湍流通量主要由热驱动。由温暖上升气流和凉爽下沉气流组成的火灾引起的热通量事件在长达一秒的周期内是相干的,而环境热通量事件主要在较长周期(超过17秒)运行。后来,当在地表附近记录到最强温度波动时,火灾引起的热通量事件在较短尺度上间歇性发生,在冠层顶部附近8至35秒的周期内开始出现凉爽扫掠,这表明火焰的影响减弱,那里的背景大气变率增加。随着火前沿的演变,对与火灾引起的湍流特征相关的特征时间尺度的更好理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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