000904135 001__ 904135
000904135 005__ 20240712100850.0
000904135 0247_ $$2doi$$a10.5194/amt-14-1977-2021
000904135 0247_ $$2ISSN$$a1867-1381
000904135 0247_ $$2ISSN$$a1867-8548
000904135 0247_ $$2Handle$$a2128/29729
000904135 0247_ $$2altmetric$$aaltmetric:101678227
000904135 0247_ $$2WOS$$aWOS:000629036900001
000904135 037__ $$aFZJ-2021-05705
000904135 082__ $$a550
000904135 1001_ $$00000-0001-9419-5432$$aWagner, Robert$$b0$$eCorresponding author
000904135 245__ $$aHigh-resolution optical constants of crystalline ammonium nitrate for infrared remote sensing of the Asian Tropopause Aerosol Layer
000904135 260__ $$aKatlenburg-Lindau$$bCopernicus$$c2021
000904135 3367_ $$2DRIVER$$aarticle
000904135 3367_ $$2DataCite$$aOutput Types/Journal article
000904135 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1641194417_4795
000904135 3367_ $$2BibTeX$$aARTICLE
000904135 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000904135 3367_ $$00$$2EndNote$$aJournal Article
000904135 520__ $$aInfrared spectroscopic observations have shown that crystalline ammonium nitrate (AN) particles are an abundant constituent of the upper tropospheric aerosol layer which is formed during the Asian summer monsoon period, the so-called Asian Tropopause Aerosol Layer (ATAL). At upper tropospheric temperatures, the thermodynamically stable phase of AN is different from that at 298 K, meaning that presently available room-temperature optical constants of AN, that is, the real and imaginary parts of the complex refractive index, cannot be applied for the quantitative analysis of these infrared measurements. In this work, we have retrieved the first low-temperature data set of optical constants for crystalline AN in the 800–6000 cm−1 wavenumber range with a spectral resolution of 0.5 cm−1. The optical constants were iteratively derived from an infrared extinction spectrum of 1 µm sized AN particles suspended in a cloud chamber at 223 K. The uncertainties of the new data set were carefully assessed in a comprehensive sensitivity analysis. We show that our data accurately fit aircraft-borne infrared measurements of ammonium nitrate particles in the ATAL.
000904135 536__ $$0G:(DE-HGF)POF4-2112$$a2112 - Climate Feedbacks (POF4-211)$$cPOF4-211$$fPOF IV$$x0
000904135 588__ $$aDataset connected to CrossRef, Journals: juser.fz-juelich.de
000904135 7001_ $$0P:(DE-HGF)0$$aTesta, Baptiste$$b1
000904135 7001_ $$00000-0002-4174-9531$$aHöpfner, Michael$$b2
000904135 7001_ $$00000-0003-0136-2428$$aKiselev, Alexei$$b3
000904135 7001_ $$0P:(DE-HGF)0$$aMöhler, Ottmar$$b4
000904135 7001_ $$0P:(DE-HGF)0$$aSaathoff, Harald$$b5
000904135 7001_ $$0P:(DE-Juel1)129105$$aUngermann, Jörn$$b6$$ufzj
000904135 7001_ $$0P:(DE-HGF)0$$aLeisner, Thomas$$b7
000904135 773__ $$0PERI:(DE-600)2505596-3$$a10.5194/amt-14-1977-2021$$gVol. 14, no. 3, p. 1977 - 1991$$n3$$p1977 - 1991$$tAtmospheric measurement techniques$$v14$$x1867-1381$$y2021
000904135 8564_ $$uhttps://juser.fz-juelich.de/record/904135/files/amt-14-1977-2021.pdf$$yOpenAccess
000904135 909CO $$ooai:juser.fz-juelich.de:904135$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000904135 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129105$$aForschungszentrum Jülich$$b6$$kFZJ
000904135 9131_ $$0G:(DE-HGF)POF4-211$$1G:(DE-HGF)POF4-210$$2G:(DE-HGF)POF4-200$$3G:(DE-HGF)POF4$$4G:(DE-HGF)POF$$9G:(DE-HGF)POF4-2112$$aDE-HGF$$bForschungsbereich Erde und Umwelt$$lErde im Wandel – Unsere Zukunft nachhaltig gestalten$$vDie Atmosphäre im globalen Wandel$$x0
000904135 9141_ $$y2021
000904135 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2021-01-31
000904135 915__ $$0LIC:(DE-HGF)CCBY4$$2HGFVOC$$aCreative Commons Attribution CC BY 4.0
000904135 915__ $$0StatID:(DE-HGF)0600$$2StatID$$aDBCoverage$$bEbsco Academic Search$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bATMOS MEAS TECH : 2019$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0700$$2StatID$$aFees$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000904135 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bASC$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0561$$2StatID$$aArticle Processing Charges$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2021-01-31
000904135 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2021-01-31
000904135 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$kIEK-7$$lStratosphäre$$x0
000904135 9801_ $$aFullTexts
000904135 980__ $$ajournal
000904135 980__ $$aVDB
000904135 980__ $$aUNRESTRICTED
000904135 980__ $$aI:(DE-Juel1)IEK-7-20101013
000904135 981__ $$aI:(DE-Juel1)ICE-4-20101013