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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP8W/34AB5BE
Repositorysid.inpe.br/mtc-m18@80/2008/11.27.12.17   (restricted access)
Last Update2008:11.27.12.21.03 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m18@80/2008/11.27.12.17.36
Metadata Last Update2022:03.05.04.19.58 (UTC) administrator
Secondary KeyINPE-15644-PRE/10369
DOI10.1016/j.atmosres.2008.10.003
ISSN0169-8095
Citation KeyMachadoLimaPintMora:2009:MuSaAp
TitleRelationship between cloud-to-ground discharge and penetrative clouds: A multi-channel satellite application
Year2009
Monthjul.
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size556 KiB
2. Context
Author1 Machado, Luiz Augusto Toledo
2 Lima, Wagner Flauber Araujo
3 Pinto Junior, Osmar
4 Morales, Carlos Augusto
Resume Identifier1 8JMKD3MGP5W/3C9JHMS
2
3 8JMKD3MGP5W/3C9JJ2E
Group1 DSA-CPT-INPE-MCT-BR
2 DSA-CPT-INPE-MCT-BR
3 DGE-CEA-INPE-MCT-BR
4 DSA-CPT-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
e-Mail Addressdeicy@cptec.inpe.br
JournalAtmospheric Research
Volume93
Number1-3
Pages304-309
History (UTC)2008-12-17 15:34:33 :: deicy -> administrator ::
2009-03-19 14:07:27 :: administrator -> deicy ::
2009-10-06 11:18:50 :: deicy -> administrator ::
2022-03-05 04:19:58 :: administrator -> marciana :: 2009
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsconvective rainfall
thunderstorm
water
lightning
penetrative clouds
AbstractThis work presents a relationship between atmospheric cloud-to-ground discharges and penetrative convective clouds. It combines Infrared and Water Vapor channels from the GOES-12 geostationary satellite with cloud-to-ground discharge data from the Brazilian Integrated Lightning Detection Network (RINDAT) during the period from January to February 2005. The difference between water vapor and infrared brightness temperature is a tracer penetrating clouds. Due to the water vapor channel's strong absorption, this difference is positive only during overshooting cases, when convective clouds penetrate the stratosphere. From this difference and the cloud-to-ground, discharge measured on the ground by RINDAT, it was possible to adjust exponential curves that relate the brightness temperature difference from these two channels to the probability of occurrence of cloud-to-ground discharges, with a very large coefficient of determination. If WV-IR brightness temperature difference is greater than - 15 K there is a large potential for cloud-to-ground discharge activity. As this difference increases the cloud-to-ground discharge probably increases, for example: if this difference is equal to zero, the probability of having at least one cloud-to-ground discharge is 10.9%, 7.0% for two, 4.4% for four, 2.7% for eight and 1.5% for sixteen cloud-to-ground discharges. Through this process, was developed a scheme that estimates the probability of occurrence of cloud-to-ground discharge over all the continental region of South America. (c) 2008 Elsevier B.V. All rights reserved.
AreaMET
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doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filemachado.pdf
User Groupadministrator
deicy
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU29DP
8JMKD3MGPCW/43SRC6S
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
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7. Description control
e-Mail (login)marciana
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