A novel rocket-borne ion mass spectrometer with large mass range: instrument description and first-flight results

dc.bibliographicCitation.firstPage983eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.lastPage993eng
dc.bibliographicCitation.volume14eng
dc.contributor.authorStude, Joan
dc.contributor.authorAufmhoff, Heinfried
dc.contributor.authorSchlager, Hans
dc.contributor.authorRapp, Markus
dc.contributor.authorArnold, Frank
dc.contributor.authorStrelnikov, Boris
dc.date.accessioned2022-03-16T11:57:02Z
dc.date.available2022-03-16T11:57:02Z
dc.date.issued2021
dc.description.abstractWe present a novel rocket-borne ion mass spectrometer named ROMARA (ROcket-borne MAss spectrometer for Research in the Atmosphere) for measuring atmospheric positive and negative ions (atomic, molecular and cluster ions) and positively and negatively charged meteor smoke particles. Our ROMARA instrument has, compared to previous rocket-borne ion mass spectrometers, a markedly larger mass range of up to m=z 2000 and a larger sensitivity, particularly for meteor smoke particle detection. The major objectives of this first ROMARA flight included the following: a functional test of the ROMARA instrument, measurements between 55 and 121 km in the mass range of atmospheric positive and negative ions, a first attempt to conduct mass spectrometric measurements in the mass range of meteor smoke particles with mass-to-charge ratios up to m=z 2000, and measurements inside a polar mesospheric winter echo layer as detected by ground-based radar. Our ROMARA measurements took place on the Arctic island of Andøya, Norway, at around noon in April 2018 and represented an integral part of the polar mesospheric winter radar echo (PMWE) rocket campaign. During the rocket flight, ROMARA was operated in a measurement mode, offering maximum sensitivity and the ability to qualitatively detect total ion signatures even beyond its mass-resolving mass range. On this first ROMARA flight we were able to meet all of our objectives. We detected atmospheric species including positive atomic, molecular and cluster ions along with negative molecular ions up to about m=z 100. Above m=z 2000, ROMARA measured strong negative-ion signatures, which are likely due to negatively charged meteor smoke particles. © 2021 Author(s).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8245
dc.identifier.urihttps://doi.org/10.34657/7283
dc.language.isoengeng
dc.publisherKatlenburg-Lindau : European Geosciences Unioneng
dc.relation.doihttps://doi.org/10.5194/amt-14-983-2021
dc.relation.essn1867-8548
dc.relation.ispartofseriesAtmospheric Measurement Techniques 14 (2021), Nr. 2eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectinstrumentationeng
dc.subjectlong range transporteng
dc.subjectmass spectrometryeng
dc.subjectmeasurement methodeng
dc.subjectHesperiseng
dc.subject.ddc550eng
dc.titleA novel rocket-borne ion mass spectrometer with large mass range: instrument description and first-flight resultseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmospheric Measurement Techniqueseng
tib.accessRightsopenAccesseng
wgl.contributorIAPeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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