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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Global Wildfire Plume-Rise Data Set and Parameterizations for Climate Model Applications
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Global Wildfire Plume-Rise Data Set and Parameterizations for Climate Model Applications

机译:全球野火羽流上升数据集和气候模式应用的参数化

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The fire plume height (smoke injection height) is an important parameter for calculating the transport and lifetime of smoke particles,which can significantly affect regional and global air quality and atmospheric radiation budget.To develop an observation-based global fire plume-rise data set,a modified one-dimensional plume-rise model was used with observation-based fire size and Maximum Fire Radiative Power (MFRP) data,which are derived from satellite fire hotspot measurements.The resulting data set captured well the observed plume height distribution derived from the Multiangle Imaging SpectroRadiometer (MISR) measurements.The fraction of fire plumes penetrating above the boundary layer is relatively low at 20% at the time of MISR observation (10:30 am LT) but increases to an average of ~55% in the late afternoon,implying that the MISR observation data sampled in late morning underestimate the average daytime fire plume heights and plume mixing into the free troposphere.Therefore,adjustments are required through dynamic modeling or parameterization of fire plume height as a function of meteorological and fire conditions when the MISR data set is applied in climate model simulations.We conducted sensitivity simulations using the Community Atmospheric Models version 5 (CAM5).Model results show that the incorporation of fire plume rise in the model tends to significantly increase fire aerosol impacted regions.We applied the offline plume-rise data to develop an online fire plume height parameterization,allowing for simulating the feedbacks of climate/weather on fire plume rise in climate models.
机译:火灾羽流高度(烟雾喷射高度)是计算烟尘颗粒运移和寿命的重要参数,可显著影响区域和全球空气质量和大气辐射收支。为建立基于观测的全球火灾羽流上升数据集,采用基于观测的火灾规模和最大火灾辐射功率(MFRP)数据,利用卫星火灾热点测量数据建立改进的一维烟羽上升模型。由此产生的数据集很好地捕获了从多角度成像光谱辐射计(MISR)测量中观测到的羽流高度分布。在MISR观测时(LT上午10:30),穿透边界层上方的火羽比例相对较低,为20%,但在下午晚些时候增加到平均~55%,这意味着在上午晚些时候采样的MISR观测数据低估了白天平均火羽高度和混入自由对流层的羽流。因此,当MISR数据集应用于气候模式模拟时,需要通过动态建模或参数化来调整火灾羽流高度作为气象和火灾条件的函数。我们使用社区大气模型第5版(CAM5)进行了灵敏度模拟。模型结果表明,在模型中加入火羽上升往往会显著增加火灾气溶胶影响区域。利用离线羽流上升数据,建立了在线火羽流高度参数化方法,模拟了气候/天气对气候模式中火羽上升的反馈。

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