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dc.contributor.authorVanderstraeten, P. Lénelle, Y.
dc.contributor.authorMeurrens, A.
dc.contributor.authorCarati, D.
dc.contributor.authorBrenig, L.
dc.contributor.authorDelcloo, A.
dc.contributor.authorOffer, Z.Y.
dc.contributor.authorZaady, E.
dc.coverage.temporal21st century
dc.date2008
dc.date.accessioned2016-03-07T16:16:59Z
dc.date.accessioned2021-12-09T09:53:57Z
dc.date.available2016-03-07T16:16:59Z
dc.date.available2021-12-09T09:53:57Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8787
dc.descriptionErosion, transport and deposition of atmospheric dust are largely determined by the nature and state of the earth's surface (the dust source) and the physical characteristics of the atmosphere. The state of the atmosphere is subject to important temporal variations related to diurnal and seasonal cycles and to synoptic conditions. The dynamic evolution of particulate concentrations measured at Brussels showed a significant peak in PM10 during 24–25 March 2007. The 4-day backward trajectories calculated for this peak attributed its cause to a dust storm that had occurred 2 days earlier in the Sahara. Chemical analysis showed a significant similarity to Saharan dust composition, primarily oxides of Si, Fe, and Al. On 29 March, another peak with a very high PM concentration and an elevated PM2.5-to-PM10 ratio was recorded in Brussels. Analysis of its PM profile showed that it was mainldy caused by formation of secondary aerosols.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesAtmospheric Environment 42
dc.titleDust storm originate from Sahara covering Western Europe
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeAtmosphere
dc.subject.freeTrajectory
dc.subject.freeContentration
dc.subject.freeParticle size
dc.subject.freeChemistry
dc.source.issueAtmospheric Environment 42
dc.source.page5489-5493
Orfeo.peerreviewedNot pertinent


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