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dc.contributor.authorRamon, D.
dc.contributor.authorBrogniez, C.
dc.contributor.authorLecomte, P.
dc.contributor.authorLenoble, J.
dc.contributor.authorVerwaerde, C.
dc.contributor.authorSimon, P.C.
dc.contributor.authorMuller, C.
dc.date1995
dc.date.accessioned2017-05-30T12:39:51Z
dc.date.available2017-05-30T12:39:51Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5579
dc.descriptionA balloon borne instrument BALLAD (balloon limb aerosol detection) has been developed at the LOA (Laboratoire d'Optique Atmospherique). It scans the Earth's limb at three wavelengths (450, 600, and 850 nm) from the float altitude between 30 - 35 km when the sun is low above the horizon; polarization is also measured in the 850 nm channel. A flight has been performed from the southwest of France on October 13, 1994 during the phase II of the SESAME (Second European Stratospheric Arctic and Mid-latitude Experiment) campaign. An analysis of the reflectances at 850 and 450 nm without polarization is presented.
dc.languageeng
dc.titleDetection of aerosols from balloon limb observations
dc.typeConference
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeAerosol detection
dc.subject.freeBalloon borne instrument BALLAD
dc.subject.freeReflectances
dc.subject.freeSESAME program
dc.subject.freeChemical analysis
dc.subject.freeLight polarization
dc.subject.freeMeteorological balloons
dc.subject.freeOptical instruments
dc.subject.freeAtmospheric aerosols
dc.source.titleProceedings of SPIE 2582: Atmospheric Sensing and Modeling II
dc.source.volume2582
dc.source.page100-109
Orfeo.peerreviewedNo
dc.identifier.doi10.1117/12.228528
dc.identifier.scopus2-s2.0-0029545501


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