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首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Long-term (1999–2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements
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Long-term (1999–2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements

机译:长期(1999-2019)在Mauna Loa,夏威夷的平坦散热醇变异,由两个共同位于典范和卫星测量

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As part of the Network for the Detection of Atmospheric Composition Change (NDACC), ground-based measurements obtained from the Jet Propulsion Laboratory (JPL) stratospheric ozone lidar and the NOAA stratospheric aerosol lidar at Mauna Loa, Hawaii, over the past 2 decades were used to investigate the impact of volcanic eruptions and pyrocumulonimbus (PyroCb) smoke plumes on the stratospheric aerosol load above Hawaii since 1999. Measurements at 355 and 532nm conducted by these two lidars revealed a color ratio of 0.5 for background aerosols and small volcanic plumes and 0.8 for a PyroCb plume recorded on September?2017. Measurements of the Nabro plume by the JPL lidar in 2011–2012 showed a lidar ratio of (64±12.7)sr at 355nm around the center of the plume. The new Global Space-based Stratospheric Aerosol Climatology (GloSSAC), Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) Level 3 and Stratospheric Aerosol and Gas Experiment III on the International Space Station (SAGE III-ISS) stratospheric aerosol datasets were compared to the ground-based lidar datasets. The intercomparison revealed a generally good agreement, with vertical profiles of extinction coefficient within 50% discrepancy between 17 and 23km above sea level (a.s.l.) and 25% above 23kma.s.l. The stratospheric aerosol depth derived from all of these datasets shows good agreement, with the largest discrepancy (20%) being observed between the new CALIOP Level 3 and the other datasets. All datasets consistently reveal a relatively quiescent period between 1999 and 2006, followed by an active period of multiple eruptions (e.g., Nabro) until early 2012. Another quiescent period, with slightly higher aerosol background, lasted until mid-2017, when a combination of extensive wildfires and multiple volcanic eruptions caused a significant increase in stratospheric aerosol loading. This loading maximized at the very end of the time period considered (fall 2019) as a result of the Raikoke eruption, the plume of which ascended to 26km altitude in less than 3 months.
机译:作为网络的一部分,用于检测大气组成变化(NDACC),从夏威夷Mauna Loa的射流推进实验室(JPL)Stratospheric臭氧LiDAR和NOAA Stratospheric气溶胶LiDAR获得的基于地基测量,在过去2年中用于探讨火山爆发和Pyrocumulonimbus(Pyrocb)烟雾羽毛在1999年以来夏威夷的平流层气溶胶负荷的影响。这两种激光器进行的355和532nm的测量显示背景气溶胶和小火山羽毛的颜色比为0.5在9月份记录的Pyrocb羽流量,2017年。 JPL LIDAR 2011-2012的Nabro羽流的测量显示了羽流中心的355nm处的(64±12.7)Sr的激光雷达比。与正交极化(Caliop)水平3和平流层气溶胶和天然气天然气和天然气实验III的新全球空间的平坦气雾气凝球学(Glossac),与国际空间站(Sage III-ISS)平流层气溶胶数据集进行基于地面的LIDAR数据集。依读的概况普遍良好的一致性,消光系数的垂直曲线在海拔17至23km之间的50%差异范围内(A.L.)和23kma.s以上25%。来自所有这些数据集的平流层气溶胶深度显示出良好的一致性,在新的卡利普3级和其他数据集之间观察到的最大差异(20%)。所有数据集始终如一地揭示了1999年和2006年之间的相对静态时期,然后是在2012年初的多次爆发(例如,NaBro)的活动期间,直到2012年初。另一个静止的时期,气溶胶背景略高,持续到2017年中期,当组合广泛的野火和多次火山爆发引起了平流层气溶胶荷载量显着增加。由于Raikoke爆发,该负荷在考虑的时间段(2019年秋季)的爆发的结果中最大化,其中羽流在不到3个月的时间内升至26km的高度。

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