Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6580
DC FieldValueLanguage
dc.contributor.authorallPrata, F.; NILU, Norwayen
dc.contributor.authorallStohl, A.; NILU, Norwayen
dc.contributor.authorallTørseth, K.; NILU, Norwayen
dc.contributor.authorallClarisse, L.; ULB, Belgiumen
dc.contributor.authorallCarn, S.; Michigan Technological University, USAen
dc.contributor.authorallPavalonis, M.; CIMSS, University of Wisconsin, USAen
dc.contributor.authorallCorradini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallMerucci, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallPiscini, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.date.accessioned2011-01-12T14:33:23Zen
dc.date.available2011-01-12T14:33:23Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6580en
dc.description.abstractEarth orbiting satellites provide an excellent means for monitoring and measuring emissions from volcanic eruptions. The recent eruption of Eyjafjallajökull in Iceland on 14 April, 2010 and the subsequent movement of the ash clouds were tracked using a variety of satellite instruments as they moved over Europe. Data from the rapid sampling (every 15 minutes) SEVIRI on Meteosat Second Generation were especially useful during this event as the thermal channels between 10–12 micron could be used to detect the ash signal and perform quantitative ash retrievals of mass loadings, optical depths and effective particle size. Higher-spatial resolution ( 1 km2) information from the MODIS sensors on NASA’s Terra and Aqua platforms were also analysed to determine ash microphysics and also to provide ash cloud top height. High-spectral resolution data from the IASI and AIRS sensors showed that initially quantities of ice, potentially with ash cores, were present, and that multi-species retrievals could be performed by exploiting the spectral content of the data. Vertically resolved ash layers were detected using the Caliop lidar on board the Calipso platform. Ash was clearly detected over Europe using the infra-red sensors with mass loadings typically in the range 0.1–5 gm-2, which for layers of 500–1000 m thickness, suggests ash concentrations in the range 0.1–10 mg m-3, and therefore represent a potential hazard to aviation.Little SO2 was detected at the start of the eruption, although both OMI and AIRS detected upper-level SO2 on 15 April. By late April and early May, 0.1–0.3 Tg (SO2) could be detected using these sensors. The wealth of satellite data available, some in near real-time, and the ability of infrared and ultra-violet sensors to detect volcanic ash and SO2 are emphasised in this presentation. The ash/aviation problem can be addressed using remote sensing measurements, validated with ground-based and air-borne, and combined with dispersion modelling. The volcanic ash threat to aviation can be ameliorated by utilising these space-based resources.en
dc.language.isoEnglishen
dc.relation.ispartofEGU 2010en
dc.subjectash retrievalen
dc.subjectvolcanic risken
dc.subjectMODISen
dc.subjectSEVIRIen
dc.subjectAIRSen
dc.subjectIASIen
dc.subjectCALIOPen
dc.subjectOMIen
dc.subjectSO2 retrievalen
dc.subjectEyjafjallajokullen
dc.titleSatellite detection of volcanic ash from Eyjafjallajökull and the threat to aviationen
dc.typeOral presentationen
dc.description.statusPublisheden
dc.subject.INGV01. Atmosphere::01.01. Atmosphere::01.01.07. Volcanic effectsen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoringen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniquesen
dc.subject.INGV04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risken
dc.description.ConferenceLocationVienna - Austriaen
dc.description.fulltextopenen
dc.contributor.authorPrata, F.en
dc.contributor.authorStohl, A.en
dc.contributor.authorTørseth, K.en
dc.contributor.authorClarisse, L.en
dc.contributor.authorCarn, S.en
dc.contributor.authorPavalonis, M.en
dc.contributor.authorCorradini, S.en
dc.contributor.authorMerucci, L.en
dc.contributor.authorPiscini, A.en
dc.contributor.departmentNILU, Norwayen
dc.contributor.departmentNILU, Norwayen
dc.contributor.departmentNILU, Norwayen
dc.contributor.departmentULB, Belgiumen
dc.contributor.departmentMichigan Technological University, USAen
dc.contributor.departmentCIMSS, University of Wisconsin, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
item.openairetypeOral presentation-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptNILU, Norway-
crisitem.author.deptNILU, Norway-
crisitem.author.deptUniversité Libre de Bruxelles-
crisitem.author.deptCIMSS, University of Wisconsin, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.orcid0000-0001-9285-9565-
crisitem.author.orcid0000-0002-0360-6660-
crisitem.author.orcid0000-0001-9432-3246-
crisitem.author.orcid0000-0001-6910-8800-
crisitem.author.orcid0000-0001-5545-3611-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent01. Atmosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Conference materials
Files in This Item:
File Description SizeFormat
EGU2010-15732.pdfAbstract38.91 kBAdobe PDFView/Open
Show simple item record

Page view(s) 50

215
checked on Apr 24, 2024

Download(s) 50

86
checked on Apr 24, 2024

Google ScholarTM

Check