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Cold Smoke: smoke-induced density currents cause unexpected smoke transport near large wildfires

机译:冷烟:浓烟引起的浓烟流导致大火附近的意外烟气传输

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The first observations of smoke-induced density currents originating from largewildfires are presented. Using a novel mobile Doppler lidar and additionalin situ measurements, we document a deep (~ 2 km) smoke-filleddensity current that propagates more than 25 km at speeds up to 4.5 m s?1 near a large forest fire in northern California. Based on theseobservations we show that the dynamics governing the spread of the smokelayer result from differential solar heating between the smoke-filled andsmoke-free portions of the atmospheric boundary layer. A calculation of thetheoretical density current speed agrees well with the observed propagationspeed. Additional lidar and photographic documentation of other smoke-filleddensity currents demonstrate that these previously unknown phenomena arerelatively common near large wildfires and can cause severe and unexpectedsmoke inundation of populated areas.
机译:提出了由大火引发的烟感密度流的首次观测。使用新颖的移动多普勒激光雷达和额外的原位测量,我们记录了深(〜2 km)的烟雾填充密度电流,该电流在大森林火灾附近以高达4.5 ms ?1 的速度传播超过25 km在加利福尼亚北部。基于这些观察,我们表明,控制烟层扩散的动力学是由大气边界层的烟气填充部分和无烟部分之间的不同太阳加热引起的。理论密度电流速度的计算与观察到的传播速度非常吻合。附加的激光雷达和其他烟雾密集流的照相记录表明,这些以前未知的现象在大山火附近相对普遍,并且可能导致人口稠密的地区发生严重的意外烟雾。

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