Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.5194/acp-20-6821-2020 |
Long-term (1999-2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements | |
Chouza, Fernando1; Leblanc, Thierry1; Barnes, John2; Brewer, Mark1; Wang, Patrick1; Koon, Darryl1 | |
2020-06-10 | |
发表期刊 | ATMOSPHERIC CHEMISTRY AND PHYSICS
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ISSN | 1680-7316 |
EISSN | 1680-7324 |
出版年 | 2020 |
卷号 | 20期号:11页码:6821-6839 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | 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 532 nm 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 355 nm around the center of the plume. The new Global Space-based Stratospheric Aerosol Climatology (G1oSSAC), 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 23 km above sea level (a.s.l.) and 25 % above 23 km a.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 exten- sive 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 26 km altitude in less than 3 months. |
领域 | 地球科学 |
收录类别 | SCI-E |
WOS记录号 | WOS:000541598700003 |
WOS关键词 | TOMSK WESTERN SIBERIA ; RAMAN LIDAR ; BACKSCATTER ; EXTINCTION ; CLIMATE ; LAYER ; SMOKE ; CONVERSIONS ; IMPACT ; PLUME |
WOS类目 | Environmental Sciences ; Meteorology & Atmospheric Sciences |
WOS研究方向 | Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences |
URL | 查看原文 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/274328 |
专题 | 地球科学 |
作者单位 | 1.CALTECH, Jet Prop Lab, Wrightwood, CA 92397 USA; 2.NOAA, ESRL, Global Monitoring Div, Boulder, CO USA |
推荐引用方式 GB/T 7714 | Chouza, Fernando,Leblanc, Thierry,Barnes, John,et al. Long-term (1999-2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2020,20(11):6821-6839. |
APA | Chouza, Fernando,Leblanc, Thierry,Barnes, John,Brewer, Mark,Wang, Patrick,&Koon, Darryl.(2020).Long-term (1999-2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements.ATMOSPHERIC CHEMISTRY AND PHYSICS,20(11),6821-6839. |
MLA | Chouza, Fernando,et al."Long-term (1999-2019) variability of stratospheric aerosol over Mauna Loa, Hawaii, as seen by two co-located lidars and satellite measurements".ATMOSPHERIC CHEMISTRY AND PHYSICS 20.11(2020):6821-6839. |
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