| 1. Identity statement | ||||
| Reference Type | Journal Article | |||
| Site | mtc-m21d.sid.inpe.br | |||
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identifier | 8JMKD3MGP3W34T/4859NGL | |||
| Repository | sid.inpe.br/mtc-m21d/2022/12.01.17.45 (restricted access) | |||
| Last Update | 2022:12.01.17.45.00 (UTC) simone | |||
| Metadata Repository | sid.inpe.br/mtc-m21d/2022/12.01.17.45.01 | |||
| Metadata Last Update | 2023:01.03.16.46.26 (UTC) administrator | |||
| DOI | 10.1007/s00704-022-04234-x | |||
| ISSN | 0177-798X | |||
| Citation Key | RaoGoAsKaReRo:2022:UnViBr | |||
| Title | A unified view of breaks in Indian, North American, and South American summer monsoons  | |||
| Year | 2022 | |||
| Month | Nov. | |||
| Access Date | 2024, June 26 | |||
| Type of Work | journal article | |||
| Secondary Type | PRE PI | |||
| Number of Files | 1 | |||
| Size | 7000 KiB | |||
| 2. Context | ||||
| Author | 1 Rao, Brahmananda Vadlamudi 2 Govardhan, Dandu 3 Ashok, Karumuri 4 Kayano, Mary Toshie 5 Reyes Fernandez, Julio Pablo 6 Rosa, Marcelo Barbio | |||
| Resume Identifier | 1 2 3 4 8JMKD3MGP5W/3C9JHST 5 8JMKD3MGP5W/3C9JHKJ 6 8JMKD3MGP5W/3C9JHNT | |||
| ORCID | 1 2 0000-0001-5159-701X | |||
| Group | 1 DIMNT-CGCT-INPE-MCTI-GOV-BR 2 3 4 DIMNT-CGCT-INPE-MCTI-GOV-BR 5 DIMNT-CGCT-INPE-MCTI-GOV-BR 6 DIMNT-CGCT-INPE-MCTI-GOV-BR | |||
| Affiliation | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 University of Hyderabad 3 University of Hyderabad 4 Instituto Nacional de Pesquisas Espaciais (INPE) 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 Instituto Nacional de Pesquisas Espaciais (INPE) | |||
| Author e-Mail Address | 1 2 govardan.d@gmail.com 3 4 5 jprf.clarice@gmail.com 6 marcelo.barbio@yahoo.com.br | |||
| Journal | Theoretical and Applied Climatology | |||
| Volume | 150 | |||
| Number | 3/4 | |||
| Pages | 1443-1461 | |||
| Secondary Mark | A1_GEOGRAFIA A1_ENGENHARIAS_I A2_INTERDISCIPLINAR A2_GEOCIÊNCIAS A2_CIÊNCIAS_AMBIENTAIS A2_CIÊNCIAS_AGRÁRIAS_I B1_BIODIVERSIDADE B1_ARQUITETURA_E_URBANISMO B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA | |||
| History (UTC) | 2022-12-01 17:45:01 :: simone -> administrator :: 2022-12-01 17:45:01 :: administrator -> simone :: 2022 2022-12-01 17:45:44 :: simone -> administrator :: 2022 2022-12-08 02:51:14 :: administrator -> simone :: 2022 2022-12-20 14:15:28 :: simone -> administrator :: 2022 2023-01-03 16:46:26 :: administrator -> simone :: 2022 | |||
| 3. Content and structure | ||||
| Is the master or a copy? | is the master | |||
| Content Stage | completed | |||
| Transferable | 1 | |||
| Content Type | External Contribution | |||
| Version Type | publisher | |||
| Abstract | The monsoon breaks in the core monsoon region of India, lasting a few days or sometimes even up to 2 weeks, are periods of low or no rainfall. Our analysis of breaks shows they are characteristically preceded by an upper-tropospheric transient blocking high over north India, which extends to low levels. The formation of this blocking high is found to be due to the penetration of mid-latitude baroclinic waves into lower latitudes. Importantly, this transient blocking high is weaker than the seasonal high at this level. The weakening of the high pressure due to the presence of this transient blocking leads to a sinking motion relative to the pre-break or post-break period, which in turn leads to a filled-up surface low, and an eventual reduction in daily rainfall. The blocking high is associated with the convergence of Eliassen-Palm fluxes, which causes the upper-level zonal westerlies to decelerate and holds the blocking high in place without being advected. Also, we find that the resonance and amplification of planetary Rossby waves play a vital role in the block formation over the northwest of India. This sequence of events, the formation of upper-level blocking high due to resonance of planetary Rossby waves at mid-latitudes followed by the break and a relative sinking over the core monsoon region, also explains the North and South American summer monsoon breaks. The entire life cycle of monsoon break formation and reversal to normal monsoon can be seen as a barotropic adiabatic cycle, analogous to the well-known midlatitude index cycle. We propose these oscillations as "Monsoon Index Cycles.". | |||
| Area | MET | |||
| Arrangement | urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > A unified view... | |||
| doc Directory Content | access | |||
| source Directory Content | there are no files | |||
| agreement Directory Content |
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| 4. Conditions of access and use | ||||
| Language | en | |||
| Target File | s00704-022-04234-x.pdf | |||
| User Group | simone | |||
| Reader Group | administrator simone | |||
| Visibility | shown | |||
| Archiving Policy | denypublisher denyfinaldraft12 | |||
| Read Permission | deny from all and allow from 150.163 | |||
| Update Permission | not transferred | |||
| 5. Allied materials | ||||
| Next Higher Units | 8JMKD3MGPCW/46KUATE | |||
| Citing Item List | sid.inpe.br/bibdigital/2022/04.03.22.23 5 sid.inpe.br/mtc-m21/2012/07.13.14.54.34 3 sid.inpe.br/mtc-m21/2012/07.13.14.53.04 2 | |||
| Dissemination | WEBSCI; PORTALCAPES; MGA. | |||
| Host Collection | urlib.net/www/2021/06.04.03.40 | |||
| 6. Notes | ||||
| Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url | |||
| 7. Description control | ||||
| e-Mail (login) | simone | |||
| update | ||||