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1. Identity statement
Reference TypeBook Section
Sitemtc-m16.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/mtc-m16@80/2006/07.03.12.59
Last Update2007:04.20.17.25.54 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m16@80/2006/07.03.12.59.50
Metadata Last Update2018:06.05.01.16.51 (UTC) administrator
Secondary KeyINPE-14666-PRE/9645
Citation KeyDeshlerABCGGHMOS:2006:NoStAe
TitleNon-volcanic stratospheric aerosol trends: 1971-2004
Year2006
Access Date2024, May 17
Secondary TypePRE LI
Number of Files1
Size30434 KiB
2. Context
Author 1 Deshler, Terry
 2 Anderson-Sprecher, Richard
 3 Barnes, John
 4 Clemesha, Barclay Robert
 5 Godin-Beekman, Sophie
 6 Grainger, Roy
 7 Hofmann, David
 8 Jä
 9 ger, Horst
10 Marsh, Steven
11 Osborn, Mary
12 Simonich, Dale Marting
Resume Identifier 1
 2
 3
 4 8JMKD3MGP5W/3C9JGKH
Group 1
 2
 3
 4 DAE-INPE-MCT-BR
Affiliation 1
 2
 3
 4 Instituto Nacional de Pesquisas Espaciais. Divisã
 5 o de Aeronomia (INPE.DAE)
EditorThomason, L
Peter, T.
Book TitleAssessment of Stratospheric Aerosol Properties (ASAP)
PublisherWorld Climate Research Program
Volume4
Pages178-218
History (UTC)2006-07-03 12:59:50 :: simone -> administrator ::
2006-09-29 03:28:31 :: administrator -> simone ::
2007-04-20 17:25:58 :: simone -> administrator ::
2018-06-05 01:16:51 :: administrator -> marciana :: 2006
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractThe existence of persistent atmospheric aerosol after volcanic eruptions must have been apparent to careful observers from early times. The reddish diffraction ring around the sun following large volcanic eruptions was first described by Sereno Bishop nine days after the eruption of Krakatoa, in late August 1883, and led to the name Bishop's ring. Less certain is that early observers suspected that aerosol persisted in the stratosphere during volcanically quiescent periods. The first published report suggesting a persistent aerosol layer in the stratosphere used purple twilight observations [Gruner and Kleinert, 1927]. Quantitative observations characterizing the altitudes, sizes, masses, and aerosol compositions involved were first provided by balloonborne impactor measurements in the late 1950s [Junge et al., 1961]. Subsequent measurements by both aircraft- and balloon-borne impactors suggested the global distribution of stratospheric aerosol [Junge and Manson, 1961; Chagnon and Junge, 1961]. On a few occasions, in addition to the impactors which measured particles > 0.1 ìm, Aitken particle counters were included on the balloon gondola. While the Aitken nuclei concentration decreased through the stratosphere, particles > 0.1 ìm had a maximum in concentration near 20 km, suggesting an aerosol source in this region [Junge et al., 1961]. These particles were large enough to create the purple twilight noted by early observers; however, recent work suggests that tropospheric aerosol must also contribute to the purple twilight in cases of a clean stratosphere [Lee and Hernandez-Andres, 2003].
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Non-volcanic stratospheric aerosol...
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/sid.inpe.br/mtc-m16@80/2006/07.03.12.59
zipped data URLhttp://urlib.net/zip/sid.inpe.br/mtc-m16@80/2006/07.03.12.59
Languageen
Target FileNon Volcanic Stratospheric.pdf
User Groupadministrator
simone
Visibilityshown
Copy HolderSID/SCD
Update Permissiontransferred to simone
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.40.54 4
DisseminationNTRSNASA; BNDEPOSITOLEGAL.
Host Collectionsid.inpe.br/banon/2003/08.15.17.40
6. Notes
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