000012593 001__ 12593
000012593 005__ 20240712100954.0
000012593 0247_ $$2DOI$$a10.1029/2010GL044056
000012593 0247_ $$2WOS$$aWOS:000281138100001
000012593 0247_ $$2Handle$$a2128/20846
000012593 037__ $$aPreJuSER-12593
000012593 041__ $$aeng
000012593 082__ $$a550
000012593 084__ $$2WoS$$aGeosciences, Multidisciplinary
000012593 1001_ $$0P:(DE-Juel1)VDB86534$$aPommrich, R.$$b0$$uFZJ
000012593 245__ $$aWhat causes the irregular cycle of the atmospheric tape recorder signal in HCN?
000012593 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2010
000012593 300__ $$aL16805
000012593 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000012593 3367_ $$2DataCite$$aOutput Types/Journal article
000012593 3367_ $$00$$2EndNote$$aJournal Article
000012593 3367_ $$2BibTeX$$aARTICLE
000012593 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000012593 3367_ $$2DRIVER$$aarticle
000012593 440_0 $$02249$$aGeophysical Research Letters$$v37$$x0094-8276
000012593 500__ $$aRecord converted from VDB: 12.11.2012
000012593 520__ $$aVariations in the mixing ratio of long-lived trace gases entering the stratosphere in the tropics are carried upward with the rising air with the signal being observable throughout the tropical lower stratosphere. This phenomenon, referred to as "atmospheric tape recorder" has previously been observed for water vapor, CO2, and CO which exhibit an annual cycle. Recently, based on Microwave Limb Sounder (MLS) and the Atmospheric Chemistry Experiment Fourier Transform Spectrometer (ACE-FTS) satellite measurements, the tape recorder signal has been observed for hydrogen cyanide (HCN) but with an approximately two-year period. Here we report on a model simulation of the HCN tape recorder for the time period 2002-2008 using the Chemical Lagrangian Model of the Stratosphere (CLaMS). The model can reproduce the observed pattern of the HCN tape recorder signal if time-resolved emissions from fires in Indonesia are used as lower boundary condition. This finding indicates that inter-annual variations in biomass burning in Indonesia, which are strongly influenced by El Nino events, control the HCN tape recorder signal. A longer time series of tropical HCN data will probably exhibit an irregular cycle rather than a regular biannual cycle. Citation: Pommrich, R., R. Muller, J.-U. Grooss, G. Gunther, P. Konopka, M. Riese, A. Heil, M. Schultz, H.-C. Pumphrey, and K. A. Walker (2010), What causes the irregular cycle of the atmospheric tape recorder signal in HCN?, Geophys. Res. Lett., 37, L16805, doi:10.1029/2010GL044056.
000012593 536__ $$0G:(DE-Juel1)FUEK491$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP23$$x0
000012593 588__ $$aDataset connected to Web of Science
000012593 650_7 $$2WoSType$$aJ
000012593 7001_ $$0P:(DE-Juel1)129138$$aMüller, R.$$b1$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)129122$$aGrooß, J.-U.$$b2$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)129123$$aGünther, G.$$b3$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)129130$$aKonopka, P.$$b4$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)129145$$aRiese, M.$$b5$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)7292$$aHeil, A.$$b6$$uFZJ
000012593 7001_ $$0P:(DE-Juel1)6952$$aSchultz, M.$$b7$$uFZJ
000012593 7001_ $$0P:(DE-HGF)0$$aPumphrey, H.-C.$$b8
000012593 7001_ $$0P:(DE-HGF)0$$aWalker, K.A.$$b9
000012593 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2010GL044056$$gVol. 37, p. L16805$$pL16805$$q37<L16805$$tGeophysical research letters$$v37$$x0094-8276$$y2010
000012593 8567_ $$uhttp://dx.doi.org/10.1029/2010GL044056
000012593 8564_ $$uhttps://juser.fz-juelich.de/record/12593/files/PDF_Pommrich.et.al2010.pdf$$yOpenAccess
000012593 8564_ $$uhttps://juser.fz-juelich.de/record/12593/files/PDF_Pommrich.et.al2010.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000012593 909CO $$ooai:juser.fz-juelich.de:12593$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000012593 9131_ $$0G:(DE-Juel1)FUEK491$$bErde und Umwelt$$kP23$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zvormals P22
000012593 9141_ $$y2010
000012593 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000012593 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000012593 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$gIEK$$kIEK-7$$lStratosphäre$$x0
000012593 9201_ $$0I:(DE-Juel1)IEK-8-20101013$$gIEK$$kIEK-8$$lTroposphäre$$x1
000012593 9201_ $$0I:(DE-82)080012_20140620$$gJARA$$kJARA-HPC$$lJülich Aachen Research Alliance - High-Performance Computing$$x2
000012593 970__ $$aVDB:(DE-Juel1)124279
000012593 9801_ $$aFullTexts
000012593 980__ $$aVDB
000012593 980__ $$aConvertedRecord
000012593 980__ $$ajournal
000012593 980__ $$aI:(DE-Juel1)IEK-7-20101013
000012593 980__ $$aI:(DE-Juel1)IEK-8-20101013
000012593 980__ $$aI:(DE-82)080012_20140620
000012593 980__ $$aUNRESTRICTED
000012593 981__ $$aI:(DE-Juel1)ICE-4-20101013
000012593 981__ $$aI:(DE-Juel1)ICE-3-20101013
000012593 981__ $$aI:(DE-Juel1)ICE-3-20101013
000012593 981__ $$aI:(DE-Juel1)IEK-8-20101013
000012593 981__ $$aI:(DE-Juel1)VDB1346