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Quantifying the mass loading of particles in an ash cloud remobilized from tephra deposits on Iceland

机译:量化从冰岛特菲拉矿床中迁移出来的灰云中颗粒的质量负荷

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pstrongAbstract./strong On 16a??17 September 2013 strong surface winds over tephra deposits in southern Iceland led to the resuspension and subsequent advection of significant quantities of volcanic ash. The resulting resuspended ash cloud was transported to the south-east over the North Atlantic Ocean and, due to clear skies at the time, was exceptionally well observed in satellite imagery. We use satellite-based measurements in combination with radiative transfer and dispersion modelling to quantify the total mass of ash resuspended during this event. Typically ash clouds from explosive eruptions are identified in satellite measurements from a negative brightness temperature difference (BTD) signal; however this technique assumes that the ash resides at high levels in the atmosphere. Due to a temperature inversion in the troposphere over southern Iceland during 16 September 2013, the resuspended ash cloud was constrained to altitudes of a??&a??span class="thinspace"/span2span class="thinspace"/spankmspan class="thinspace"/spana.s.l. We show that a positive BTD signal can instead be used to identify ash-containing pixels from satellite measurements. The timing and location of the ash cloud identified using this technique from measurements made by the Visible Infrared Imaging Radiometer Suite (VIIRS) on board the Suomi National Polar-orbiting Partnership (NPP) satellite agree well with model predictions using the dispersion model NAME (Numerical Atmospheric-dispersion Modelling Environment). Total column mass loadings are determined from the VIIRS data using an optimal estimation technique which accounts for the low altitude of the resuspended ash cloud and are used to calibrate the emission rate in the resuspended ash scheme in NAME. Considering the tephra deposits from the recent eruptions of Eyjafjallaj??kull and Gr?-msv??tn as the potential source area for resuspension for this event, we estimate that a??a??a??span class="thinspace"/span0.2span class="thinspace"/spanTg of ash was remobilized during 16a??17 September 2013./p.
机译:> >摘要。2013年9月16日至17日,冰岛南部南部的特菲拉矿床上空强风,导致大量火山灰重新悬浮并随后平流。产生的重悬灰云被运送到北大西洋的东南部,由于当时天空晴朗,在卫星图像中观察得非常好。我们将基于卫星的测量与辐射传输和弥散模型结合使用,以量化此事件期间重悬的灰分的总质量。通常,在卫星测量中会根据负的亮度温度差(BTD)信号来识别爆炸性爆发产生的灰云。但是,该技术假定灰烬在大气中的含量很高。由于2013年9月16日冰岛南部对流层的温度反转,重悬的灰云被限制在a ?? ?? class =“ thinspace”> 2 class = “ thinspace”> km class =“ thinspace”> asl我们显示正的BTD信号可以代替卫星测量来识别含灰像素。使用此技术从Suomi国家极地轨道合作伙伴(NPP)卫星上的可见红外成像辐射计套件(VIIRS)进行的测量中确定的灰云的时间和位置与使用色散模型NAME(Numerical大气弥散建模环境)。使用最佳估算技术根据VIIRS数据确定总柱质量,该估算技术考虑了重悬灰烬云的低海拔高度,并用于校准NAME中重悬灰烬方案的排放速率。考虑到Eyjafjallaj ?? kull和Gr?-msv ?? tn最近爆发的提弗拉沉积物是该事件的潜在重悬源区,我们估计a ?? a ?? a ?? class =“ thinspace “> 0.2 class =” thinspace“> Tg灰烬在2013年9月17日至17日期间动员。

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