Application of linear polarized light for the discrimination of frozen and liquid droplets in ice nucleation experiments

dc.bibliographicCitation.firstPage1041eng
dc.bibliographicCitation.issue4eng
dc.bibliographicCitation.lastPage1052eng
dc.bibliographicCitation.volume6
dc.contributor.authorClauss, T.
dc.contributor.authorKiselev, A.
dc.contributor.authorHartmann, S.
dc.contributor.authorAugustin, S.
dc.contributor.authorPfeifer, S.
dc.contributor.authorNiedermeier, D.
dc.contributor.authorWex, H.
dc.contributor.authorStratmann, F.
dc.date.accessioned2018-01-05T11:15:07Z
dc.date.available2019-06-26T17:20:46Z
dc.date.issued2013
dc.description.abstractWe report on the development and test results of the new optical particle counter TOPS-Ice (Thermo-stabilized Optical Particle Spectrometer for the detection of Ice). The instrument uses measurements of the cross-polarized scattered light by single particles into the near-forward direction (42.5° ± 12.7°) to distinguish between spherical and non-spherical particles. This approach allows the differentiation between liquid water droplets (spherical) and ice particles (non-spherical) having similar volume-equivalent sizes and therefore can be used to determine the fraction of frozen droplets in a typical immersion freezing experiment. We show that the numerical simulation of the light scattered on non-spherical particles (spheroids in random orientation) considering the actual scattering geometry used in the instrument supports the validity of the approach, even though the cross-polarized component of the light scattered by spherical droplets does not vanish in this scattering angle. For the separation of the ice particle mode from the liquid droplet mode, we use the width of the pulse detected in the depolarization channel instead of the pulse height. Exploiting the intrinsic relationship between pulse height and pulse width for Gaussian pulses allows us to calculate the fraction of frozen droplets even if the liquid droplet mode dominates the particle ensemble. We present test results obtained with TOPS-Ice in the immersion freezing experiments at the laminar diffusion chamber LACIS (Leipzig Aerosol Cloud Interaction Simulator) and demonstrate the excellent agreement with the data obtained in similar experiments with a different optical instrument. Finally, the advantages of using the cross-polarized light measurements for the differentiation of liquid and frozen droplets in the realistic immersion freezing experiments are discussed.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/803
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/802
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/amt-6-1041-2013
dc.relation.ispartofseriesAtmospheric Measurement Techniques, Volume 6, Issue 4, Page 1041-1052eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectdata seteng
dc.subjectdiscriminant analysiseng
dc.subjectdropleteng
dc.subjectexperimental studyeng
dc.subjectfreezingeng
dc.subjectinstrumentationeng
dc.subjectlight effecteng
dc.subjectlight scatteringeng
dc.subjectlinearityeng
dc.subjectnucleationeng
dc.subjectpolarizationeng
dc.subject.ddc550eng
dc.titleApplication of linear polarized light for the discrimination of frozen and liquid droplets in ice nucleation experimentseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
amt-6-1041-2013.pdf
Size:
1.89 MB
Format:
Adobe Portable Document Format
Description: