| 1. Identity statement | |
| Reference Type | Journal Article |
| Site | mtc-m16b.sid.inpe.br |
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
| Identifier | x6e6X3pFwXQZ3DUS8rS5/CdyFs |
| Repository | cptec.inpe.br/walmeida/2004/05.21.08.40 (restricted access) |
| Last Update | 2004:07.08.03.00.00 (UTC) administrator |
| Metadata Repository | cptec.inpe.br/walmeida/2004/05.21.08.40.28 |
| Metadata Last Update | 2021:02.10.18.59.55 (UTC) administrator |
| Secondary Key | INPE-10678-PRE/6140 |
| ISSN | 0377-0265 |
| Citation Key | BonattiVadl:1999:MePeTh |
| Title | Meso-scale perturbations and thermohaline fronts in the south atlantic ocean  |
| Year | 1999 |
| Month | aug. |
| Access Date | 2024, Apr. 28 |
| Secondary Type | PRE PI |
| Number of Files | 1 |
| Size | 1 KiB |
| 2. Context | |
| Author | 1 Bonatti, Jose Paulo 2 Vadlamudi, Brahmananda Rao |
| Group | 1 DMD-INPE-MCT-BR |
| Affiliation | 1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil |
| e-Mail Address | fabia@cptec.inpe.br |
| Journal | Dynamics of Atmospheres and Oceans |
| Volume | 30 |
| Number | 1 |
| Pages | 1-24 |
| History (UTC) | 2008-06-10 19:46:20 :: administrator -> estagiario :: 2010-05-11 16:53:15 :: estagiario -> administrator :: 2021-02-10 18:59:55 :: administrator -> marciana :: 1999 |
| 3. Content and structure | |
| Is the master or a copy? | is the master |
| Content Stage | completed |
| Transferable | 1 |
| Content Type | External Contribution |
| Keywords | oceanic thermal rings non-linear model amplitude |
| Abstract | A linear quasi-geostrophic model and a non-linear balanced model are used to study the properties of the oceanic baroclinic waves. From a linear point of view, the oceanic meso-scale (200-400 km) disturbances found near the Brazil and Falkland currents confluence zone seem to he generated by baroclinic instability. Non-geostrophic and non-linear effects due to a single original wave are superimposed on the linear fields associated with the most unstable wave. Characteristics very similar to observations are obtained in the evolution to finite amplitude. The evolution of oceanic thermal rings is very well reproduced by the non-linear model. However, the stage of saturation is not reached in the model results since the feedback to the thermal basic state is not included. (C) 1999 Elsevier Science B.V. All rights reserved. |
| Area | MET |
| Arrangement | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Meso-scale perturbations and... |
| doc Directory Content | access |
| source Directory Content | there are no files |
| agreement Directory Content | there are no files |
| 4. Conditions of access and use | |
| Language | en |
| Target File | portal.cgi?DestApp=WOS&Func=Frame |
| User Group | administrator |
| Visibility | shown |
| Copy Holder | SID/SCD |
| Archiving Policy | denypublisher denyfinaldraft24 |
| Read Permission | deny from all and allow from 150.163 |
| 5. Allied materials | |
| Next Higher Units | 8JMKD3MGPCW/43SKC35 |
| URL (untrusted data) | http://isi3.isiknowledge.com/portal.cgi?DestApp=WOS&Func=Frame |
| Dissemination | WEBSCI |
| Host Collection | cptec.inpe.br/walmeida/2003/04.25.17.12 |
| 6. Notes | |
| Empty Fields | alternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork versiontype |
| 7. Description control | |
| e-Mail (login) | marciana |
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