| dc.contributor.author | Sawamura, P | |
| dc.contributor.author | Vernier, J. E. | |
| dc.contributor.author | Barnes, J. E. | |
| dc.contributor.author | Welton, E. J. | |
| dc.contributor.author | Alados Arboledas, Lucas | |
| dc.contributor.author | Navas Guzmán, Francisco | |
| dc.contributor.author | Pappalardo, G | |
| dc.contributor.author | Mona, L. | |
| dc.contributor.author | Madonna, F. | |
| dc.contributor.author | Lange, D | |
| dc.contributor.author | Sicard, M. | |
| dc.contributor.author | Godin-Beekmann, S. | |
| dc.contributor.author | Payene, G. | |
| dc.contributor.author | Wang, Z. | |
| dc.contributor.author | Hu, S. | |
| dc.contributor.author | Tripathi, S. N. | |
| dc.contributor.author | Córdoba-Jabonero, Carmen | |
| dc.contributor.author | Hoff, R. M. | |
| dc.date.accessioned | 2025-01-28T08:51:09Z | |
| dc.date.available | 2025-01-28T08:51:09Z | |
| dc.date.issued | 2012-08-06 | |
| dc.identifier.citation | Sawamura, P. et al. Stratospheric AOD after the 2011 eruption of Nabro volcano measured by lidars over the Northern Hemisphere, Environmental Research Letters, 7, 2012. 034013,1-9, doi:10.1088/1748-9326/7/3/034013 | es_ES |
| dc.identifier.uri | https://hdl.handle.net/10481/100659 | |
| dc.description | Lidar work at UMBC was funded by grant
NNX10AR38G (DISCOVER-AQ). The NASA Micro-Pulse
Lidar Network is funded by the NASA Earth Observing
System and Radiation Sciences Program. Lidar work at the
Hefei site was funded by the National Key Basic Research
Project of China under Grant No. 2007FY110700. Lidar
work at Universidad de Granada was funded by grants
CGL2010-18782 and P10-RNM-6299. The EARLINET
stations are funded by the EU FP7 Project ‘ACTRIS’. SNT
was supported under the program, Changing Water Cycle
funded jointly by Ministry of Earth Sciences, India and
Natural Environment Research Council, UK. The OHP lidar
measurements are funded by CNRS INSU. | es_ES |
| dc.description.abstract | Nabro volcano (13.37 N, 41.70 E) in Eritrea erupted on 13 June 2011 generating a layer of sulfate aerosols that persisted in the stratosphere for months. For the first time we report on ground-based lidar observations of the same event from every continent in the Northern Hemisphere, taking advantage of the synergy between global lidar networks such as EARLINET, MPLNET and NDACC with independent lidar groups and satellite CALIPSO to track the evolution of the stratospheric aerosol layer in various parts of the globe. The globally averaged aerosol optical depth (AOD) due to the stratospheric vol- canic aerosol layers was of the order of 0.018±0.009 at 532 nm, ranging from 0.003 to 0.04. Compared to the total column AOD from the available collocated AERONET stations, the stratospheric contribution varied from 2% to 23% at 532 nm. | es_ES |
| dc.description.sponsorship | NNX10AR38G (DISCOVER-AQ) | es_ES |
| dc.description.sponsorship | NASA Earth Observing System and Radiation Sciences Program | es_ES |
| dc.description.sponsorship | National Key Basic Research Project of China 2007FY110700 | es_ES |
| dc.description.sponsorship | Universidad de Granada CGL2010-18782, P10-RNM-6299 | es_ES |
| dc.description.sponsorship | EU FP7 Project ‘ACTRIS’ | es_ES |
| dc.description.sponsorship | Ministry of Earth Sciences, India | es_ES |
| dc.description.sponsorship | Natural Environment Research Council, UK | es_ES |
| dc.description.sponsorship | CNRS INSU | es_ES |
| dc.language.iso | eng | es_ES |
| dc.publisher | IOP Science | es_ES |
| dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internacional | * |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | * |
| dc.title | Stratospheric AOD after the 2011 eruption of Nabro volcano measured by lidars over the Northern Hemisphere | es_ES |
| dc.type | journal article | es_ES |
| dc.rights.accessRights | open access | es_ES |
| dc.identifier.doi | 10.1088/1748-9326/7/3/034013 | |
| dc.type.hasVersion | VoR | es_ES |