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Gas flaring activity and black carbon emissions in 2017 derived from the Sentinel-3A Sea and Land Surface Temperature Radiometer

机译:2017年燃气辐射活动和黑碳排放源自哨兵-3A海和陆地温度辐射计

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Gas flares are a regionally and globally significant source of atmospheric pollutants. They can be detected by satellite remote sensing. We calculate the global flared gas volume and black carbon emissions in 2017 by applying (1)?a previously developed hot spot detection and characterisation algorithm to all observations of the Sea and Land Surface Temperature Radiometer (SLSTR) instrument on board the Copernicus satellite Sentinel-3A and (2)?newly developed filters for identifying gas flares and corrections for calculating both flared gas volumes (billion cubic metres, BCM) and black carbon (BC) emissions (g). The filter to discriminate gas flares from other hot spots uses the observed hot spot characteristics in terms of temperature and persistence. A regression function is used to correct for the variability of detection opportunities. A total of 6232 flaring sites are identified worldwide. The best estimates of the annual flared gas volume and the BC emissions are 129 BCM with a confidence interval of [35, 419 BCM] and 73 Gg with a confidence interval of [20, 239 Gg], respectively. Comparison of our activity (i.e. BCM) results with those of the Visible Infrared Imaging Radiometer Suite (VIIRS) Nightfire data set and SWIR-based calculations show general agreement but distinct differences in several details. The calculation of black carbon emissions using our gas flaring data set with a newly developed dynamic assignment of emission factors lie in the range of recently published black carbon inventories, albeit towards the lower end. The data presented here can therefore be used e.g. in atmospheric dispersion simulations. The advantage of using our algorithm with Sentinel-3 data lies in the previously demonstrated ability to detect and quantify small flares, the long-term data availability from the Copernicus programme, and the increased detection opportunity of global gas flare monitoring when used in conjunction with the VIIRS instruments. The flaring activity and related black carbon emissions are available as “GFlaringS3” on the Emissions of atmospheric Compounds and Compilation of Ancillary Data (ECCAD) website (https://doi.org/10.25326/19, Caseiro and Kaiser,?2019).
机译:气体耀斑是一个地区和大气污染物的全球显著来源。它们可以通过卫星遥感来检测。我们通过对板应用(1)?以前开发的热点检测和表征算法对海洋和陆地表面温度辐射计的所有观测(SLSTR)仪器哥白尼卫星哨兵计算,2017年全球火炬气的体积和黑碳排放量图3A和(2)→新开发的过滤器,用于识别气体耀斑和修正用于计算两个张开的气体体积(十亿立方米,BCM)和黑碳(BC)的排放量(克)。从其他热点判别废气燃烧过滤器使用被观察者热点特性的温度和持久性方面。回归函数用于校正的检测机会的可变性。共有6232位燃烧在全球范围内确定。每年的火炬气的体积的最佳估计和BC排放129与BCM [35,419 BCM]和73千兆克具有[20,239千兆克]分别的置信区间,的置信区间。我们的活动比较(即BCM)的结果与可见红外成像辐射计套件(VIIRS)Nightfire数据集和基于SWIR - 计算显示普遍,但在一些细节明显差异。使用我们的天然气燃烧用数据的发射因子的新开发的动态分配设置黑色碳排放的计算在于最近出版的黑色碳清单的范围内,尽管朝向下端。这里介绍的数据,因此可以例如使用在大气扩散模拟。使用我们的哨兵-3数据谎言算法在前面演示检测和定量小耀斑能力的优势,从哥白尼计划长期数据的可用性,以及全球天然气的增加检测机会火炬结合使用时,监控该仪器VIIRS。扩口活动和相关的黑碳排放量可作为大气化合物和辅助数据(ECCAD)网站的编辑(https://doi.org/10.25326/19,Caseiro和Kaiser,?2019)的排放量“GFlaringS3”。

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