首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Daily and 3‐hourly variability in global fire emissions and consequences for atmospheric model predictions of carbon monoxide
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Daily and 3‐hourly variability in global fire emissions and consequences for atmospheric model predictions of carbon monoxide

机译:全球火灾排放的每日和每三个小时变化以及一氧化碳的大气模型预测的后果

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Attribution of the causes of atmospheric trace gas and aerosol variability often requires the use of high resolution time series of anthropogenic and natural emissions inventories. Here we developed an approach for representing synoptic‐ and diurnal‐scale temporal variability in fire emissions for the Global Fire Emissions Database version 3 (GFED3). We disaggregated monthly GFED3 emissions during 2003–2009 to a daily time step using Moderate Resolution Imaging Spectroradiometer (MODIS)‐derived measurements of active fires from Terra and Aqua satellites. In parallel, mean diurnal cycles were constructed from Geostationary Operational Environmental Satellite (GOES) Wildfire Automated Biomass Burning Algorithm (WF_ABBA) active fire observations. Daily variability in fires varied considerably across different biomes, with short but intense periods of daily emissions in boreal ecosystems and lower intensity (but more continuous) periods of burning in savannas. These patterns were consistent with earlier field and modeling work characterizing fire behavior dynamics in different ecosystems. On diurnal timescales, our analysis of the GOES WF_ABBA active fires indicated that fires in savannas, grasslands, and croplands occurred earlier in the day as compared to fires in nearby forests. Comparison with Total Carbon Column Observing Network (TCCON) and Measurements of Pollution in the Troposphere (MOPITT) column CO observations provided evidence that including daily variability in emissions moderately improved atmospheric model simulations, particularly during the fire season and near regions with high levels of biomass burning. The high temporal resolution estimates of fire emissions developed here may ultimately reduce uncertainties related to fire contributions to atmospheric trace gases and aerosols. Important future directions include reconciling top‐down and bottom up estimates of fire radiative power and integrating burned area and active fire time series from multiple satellite sensors to improve daily emissions estimates.
机译:大气痕量气体和气溶胶变异性原因的归因通常需要使用人为和自然排放清单的高分辨率时间序列。在这里,我们为全球火灾排放数据库第3版(GFED3)开发了一种方法来表示天气排放的天气尺度和昼夜尺度的时间变化。我们使用源自中等分辨率成像光谱仪(MODIS)的Terra和Aqua卫星主动火源测量,将2003-2009年的GFED3每月排放量细分为每日时间步长。同时,从对地静止作战环境卫星(GOES)野火自动生物质燃烧算法(WF_ABBA)主动火观测中构造了平均日循环。在不同的生物群落中,火的日变化性差异很大,在北方生态系统中日排放量短而强烈,而在稀树草原燃烧的强度低(但更连续)。这些模式与早期野外研究和建模工作相一致,这些工作表征了不同生态系统中火灾行为的动态。在昼夜尺度上,我们对GOES WF_ABBA活跃火灾的分析表明,与附近森林的火灾相比,大草原,草原和农田的火灾是在当天早些时候发生的。与总碳柱观测网络(TCCON)的比较和对流层污染的测量(MOPITT)柱的CO观测提供了证据,包括排放量的每日变化适度改善了大气模型模拟,尤其是在火季和生物量水平较高的地区燃烧。此处对火气排放的高时间分辨率估算可以最终减少与火对大气中痕量气体和气溶胶的贡献有关的不确定性。未来的重要方向包括协调自上而下和自下而上的火辐射功率估算值,并整合来自多个卫星传感器的燃烧面积和活跃起火时间序列,以改善每日排放量估算值。

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