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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br (namespace prefix: upn:3Q3U5H8)
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/42BUF4S
Repositorysid.inpe.br/mtc-m21c/2020/04.20.11.01   (restricted access)
Last Update2020:04.20.11.01.40 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2020/04.20.11.01.40
Metadata Last Update2022:01.04.01.35.05 (UTC) administrator
DOI10.1016/j.jastp.2020.105272
ISSN1364-6826
Citation KeySousaPMSPRSH:2020:OzTrEq
TitleOzone trends on equatorial and tropical regions of South America using Dobson spectrophotometer, TOMS and OMI satellites instruments
Year2020
MonthJuly
Access Date2025, Dec. 08
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2054 KiB
2. Context
Author1 Sousa, C. T.
2 Paes Leme, Neusa Maria
3 Martins, Maria Paulete Pereira
4 Silva, F. R.
5 Penha, Tercio Luiz Bezerra
6 Rodrigues, Nilson Luís
7 Silva, E. L.
8 Hoelzemann, J. J.
Resume Identifier1
2 8JMKD3MGP5W/3C9JHUP
Group1
2 CRCRN-COCRE-INPE-MCTIC-GOV-BR
3 CRCRN-COCRE-INPE-MCTIC-GOV-BR
4
5 CRCRN-COCRE-INPE-MCTIC-GOV-BR
6 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
Affiliation1 Universidade Federal do Rio Grande do Norte (UFRN)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal do Rio Grande do Norte (UFRN)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Instituto Nacional de Pesquisas Espaciais (INPE)
8 Universidade Federal do Rio Grande do Norte (UFRN)
Author e-Mail Address1
2
3 maria.paulete@inpe.br
4
5 tercio.penha@inpe.br
6 nilson.filho@inpe.br
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume203
Pagese105272
Secondary MarkA1_ENGENHARIAS_I A2_GEOCIÊNCIAS A2_ENGENHARIAS_III B1_INTERDISCIPLINAR B1_ENGENHARIAS_IV B1_BIODIVERSIDADE B2_ASTRONOMIA_/_FÍSICA C_CIÊNCIAS_BIOLÓGICAS_I
Host Collectionurlib.net/www/2017/11.22.19.04 upn:3Q3U5H8
History (UTC)2020-04-20 11:01:40 :: simone -> administrator ::
2020-04-20 11:01:41 :: administrator -> simone :: 2020
2020-04-20 11:02:20 :: simone -> administrator :: 2020
2022-01-04 01:35:05 :: administrator -> simone :: 2020
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsDobson spectrophotometer
Ozone trend
TOMS
OMI
Total ozone content
Ozone seasonal cycle
AbstractThe ozone layer filters solar ultraviolet radiation and is affected by several photochemical and dynamical processes in the atmosphere. Stratospheric ozone formation takes place primarily in tropical regions and it is the consequence of reactions between atmospheric oxygen and the ultraviolet solar radiation. For the purpose of this paper, the atmospheric TOC (Total Ozone Content) measurements are calculated using Dobson spectrophotometers, in conjunction of satellite data of TOMS (Total Ozone Mapping Spectrometer), and OMI (Ozone Monitoring Instrument), at Cachoeira Paulista (22.7oS, 45.0oW) (CP) and Natal (5.8oS, 35.2oW) (NT), Brazil. The time series considered extend from 1974 to 2013 for CP and from 1978 to 2013 for NT. The mean differences in ozone values between Dobson and TOMS, and between Dobson and OMI, are about 3% and 2%, respectively. The correlations of the Dobson spectrophotometers with TOMS are inferior to the correlations of Dobson to OMI data, due to the improved retrieval and algorithm of the more recent OMI instrument. The observed long-term ozone trends obtained for CP and NT with Dobsons, are: −2.76%, for the period of 19742013, and -0.78%, for the period of 19782013, respectively. The trend in TOC per decade is of −0.71 ± 0.4% at CP, and of −0.22 ± 0.2%, at NT. The estimated seasonal trends for CP in June-July-August are −3.3%, compared to NT, which yields −1% in the same period. NT seasonal trend for December-January-February is −1.3%. This shows that there is a more significant decrease at CP than at NT, which agrees with the fact that the most active ozone production occurs near the equator. The average ozone amounts were 268.3 ± 13.1 DU for CP and 265.9 ± 10.9 DU for NT, and a seasonal cycle with a minimum of 256.0 DU at CP and NT in autumn and maximum of 283 DU at CP and 279 DU at NT in spring, of southern hemisphere.
AreaMET
Arrangement 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CRCRN > Ozone trends on...
Arrangement 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Ozone trends on...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Content
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4. Conditions of access and use
Languageen
Target Filesousa_ozone.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EUAPES
8JMKD3MGPCW/3EUPEJL
Citing Item Listsid.inpe.br/bibdigital/2013/10.06.18.03 - 51
sid.inpe.br/bibdigital/2013/10.03.20.46 - 49
sid.inpe.br/mtc-m21/2012/07.13.14.57.12 - 8
DisseminationWEBSCI; PORTALCAPES; AGU; COMPENDEX; SCOPUS.
6. Notes
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7. Description control
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