DSpace logo

Use este identificador para citar ou linkar para este item: http://repositorioinstitucional.uea.edu.br//handle/riuea/4002
Registro completo de metadados
Campo DCValorIdioma
dc.contributor.authorAnguelova, Mira Assenova-
dc.date.available2022-06-13-
dc.date.available2022-06-08T18:01:59Z-
dc.date.issued2022-05-24-
dc.identifier.citationANGUELOVA, Mira Assenova. Diferenças entre as evoluções temporais dos ENOS plurianuais e de único ano: Impactos na precipitação da América do Sul tropical. 2022. Trabalho de Conclusão de Curso (Bacharel em Meteorologia). Universidade do Estado do Amazonas, 2022.pt_BR
dc.identifier.urihttp://repositorioinstitucional.uea.edu.br//handle/riuea/4002-
dc.description.abstractThe present work seeks to characterize and point out the differences in the patterns of evolution el Niño-Southern Oscillation (ENOS) events lasting a single year, defined as annual, and long-term, as multi-annual, through the analysis of the Temperature of Surface of the Sea, as well as verify the influence of such events on precipitation in the Tropical South America. To this, two contrasting events, in terms of the duration of event, both for the positive phase of ENOS (El Niño) and for the negative phase (La Niña), were selected for case studies. Separate analysis of each of the events suggested that ENOS events have different characteristics in relation to intensity and persistence of anomalies when comparatoring the first and second year of Events. In addition, changes in the atmospheric patterns of tropical teleconnections during the the first and second year of the events impact differently on the precipitation of America Tropical South.pt_BR
dc.languageporpt_BR
dc.publisherUniversidade do Estado do Amazonaspt_BR
dc.rightsAcesso Abertopt_BR
dc.subjectEl Niño-Oscilação Sulpt_BR
dc.subjectVariabilidade interanualpt_BR
dc.subjectAmérica do Sul.pt_BR
dc.subjectEl Niño-Southern Oscillationpt_BR
dc.subjectInterannual Variabilitypt_BR
dc.subjectSouth Americapt_BR
dc.titleDiferenças entre as evoluções temporais dos ENOS plurianuais e de único ano: Impactos na precipitação da América do Sul tropicapt_BR
dc.title.alternativeDifferences between the time developments of multiannual AND single-year impacts on rainfall in South America tropicapt_BR
dc.typeTrabalho de Conclusão de Cursopt_BR
dc.date.accessioned2022-06-08T18:01:59Z-
dc.creator.ID5220157531040597pt_BR
dc.contributor.advisor1Souza, Rita Valéria Andreoli de-
dc.contributor.advisor1ID5550289805439528pt_BR
dc.contributor.advisor1Latteshttp://lattes.cnpq.br/5550289805439528pt_BR
dc.contributor.referee1Souza, Jaidete Monteiro de-
dc.contributor.referee1ID9120546033182086pt_BR
dc.contributor.referee1Latteshttp://lattes.cnpq.br/9120546033182086pt_BR
dc.contributor.referee2Souza, Rodrigo Augusto Ferreira de-
dc.contributor.referee2ID5622102962091766pt_BR
dc.contributor.referee2Latteshttp://lattes.cnpq.br/5622102962091766pt_BR
dc.creator.Latteshttp://lattes.cnpq.br/5220157531040597pt_BR
dc.description.resumoO presente trabalho busca caracterizar e apontar as diferenças nos padrões de evolução dos eventos de El Niño-Oscilação Sul (ENOS) com duração de um único ano, definidos como anuais, e com duração prolongada, como plurianuais, através da análise da Temperatura da Superfície do Mar, bem como verificar a influência de tais eventos sobre a precipitação na América do Sul Tropical. Para isto, dois eventos contrastantes, em termos de duração de evento, tanto para a fase positiva do ENOS (El Niño) quanto para a fase negativa (La Niña), foram selecionados para estudos de caso. A análise separada de cada um dos eventos selecionados sugeriu que os eventos ENOS apresentam características diferentes em relação a intensidade e persistência das anomalias quando comparamos o primeiro e segundo ano dos eventos. Além disso, mudanças nos padrões atmosféricos de teleconexões tropicais durante o primeiro e segundo ano dos eventos impactam de maneira diferente na precipitação da América do Sul Tropical.pt_BR
dc.publisher.countryBrasilpt_BR
dc.relation.referencesAceituno, P., 1992. El Nino, the Southern Oscillation, and ENSO: Confusing Names for a Complex Ocean-Atmosphere Interaction. Bulletin American Meteorological Society, Vol. 73, No. 4 Alexander, M. A.; Bladé I; Newman, M.; Lazante, J. R.; Lau, N.; Scot, J.D. 2002. The atmospheric bridge: the influence of ENSO teleconnections on air-sea interaction over the global oceans. Journal of Climate, 15:2205-2231. DOI: https://doi.org/10.1175/1520- 0442(2002)015<2205:TABTIO>2.0.CO;2 Berlage, H. P., 1966: The Southern Oscillation and World Weather. Koninklijk Nederlands Meteorologisch Instituut, Mededelingen en Verhandelingen No. 88, 152 pp. Bjerknes, J., 1966: A possible response of the atmospheric Hadley cell to equatorial anomalies of ocean temperature. Tellus, 18, 820-829. DOI: https://doi.org/10.3402/tellusa.v18i4.9712 Bjerknes, J. A. 1969. Atmospheric teleconnections from the equatorial Pacific. Monthly Weather Review 97: 163–172. DOI: https://doi.org/10.1175/1520- 0493(1969)097<0163:ATFTEP>2.3.CO;2 Boyin Huang, Peter W. Thorne, Viva F. Banzon, Tim Boyer, Gennady Chepurin, Jay H. Lawrimore, Matthew J. Menne, Thomas M. Smith, Russell S. Vose, and Huai-Min Zhang. 2017. NOAA Extended Reconstructed Sea Surface Temperature (ERSST), Version 5. NOAA National Centers for Environmental Information. DOI:10.7289/V5T72FNM. Bronnimann, S. 2007. Impact of El Niño – Southern Oscillation on European Climate. Rev. Geophys., 45, RG3003, DOI:10.1029/2006RG000199 Cane, M. A., and S. E. Zebiak, 1985. A theory for El Niño and the Southern Oscillation, Science, 228, 1085-1087. DOI: https://doi.org/10.1126/science.228.4703.1085 44 Chao, Y., and S. G. H. Philander, 1993. On the structure of the Southern Oscillation, J. Clim., 6, 450-469. DOI: https://doi.org/10.1175/1520-0442(1993)006<0449:OTSOTS>2.0.CO;2 C. A. S. Coelho, C. B. Uvo, T. Ambrizzi. 2002. Exploring the impacts of the tropical Pacific SST on the precipitation patterns over South America during ENSO periods. Theoretical and Applied Climatology volume 71, pages 185–197. https://doi.org/10.1007/s007040200004 Curtis, S., 2008. The El Niño–Southern Oscillation and Global Precipitation. Geography Compass 2/3 (2008): 600–619, 10.1111/j.1749-8198.2008.00105.x E. Kalnay, M. Kanamitsu, R. Kistler, W. Collins, D. Deaven, L. Gandin, M. Iredell, S. Saha, G. White, J. Woollen, Y. Zhu, M. Chelliah, W. Ebisuzaki, W. Higgins, J. Janowiak, K. C. Mo, C. Ropelewski, J. Wang, A. Leetmaa, R. Reynolds, Roy Jenne, and Dennis Joseph. 1996. The NCEP/NCAR 40-Year Reanalysis Project. American Meteorological Society, Vol. 77, No. 3. https://doi.org/10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 Gonzalez, R. A.; Andreoli, R. V.; Cândido, L. A.; Kayano, M. T.; Souza, R. A. F. 2013. A influência do evento El Niño – Oscilação Sul e Atlântico Equatorial na precipitação sobre as regiões norte e nordeste da América do Sul. Acta Amazonica, Vol. 43(4): 469-480. DOI: 10.1590/S0044-59672013000400009 A.M. Grimm. 2003. The El Niño Impact on the Summer Monsoon in Brazil: Regional Processes versus Remote Influences. Journal of Climate, Vol. 16: Issue 2, p. 263-280. https://doi.org/10.1175/1520-0442(2003)016<0263:TENIOT>2.0.CO;2 A.M. Grimm. 2004. How do La Niña events disturb the summer monsoon system in Brazil? Climate Dynamics volume 22, pages 123–138. https://doi.org/10.1007/s00382-003-0368-7 Holton, J.R. 2004. Introduction to Dynamic Meteorology. 4th Edition, Elsevier, Amsterdam, 535 p. 45 Huang, B.; Schopf, P. S.; Pan, Z. 2002. The ENSO effect on the tropical Atlantic variability: A regionally coupled model study. Geophysical Research Letters, Vol. 29, No. 21, 2039. DOI: 10.1029/2002GL014872 Julian, P. R.; Chervin, R. M., 1978. A Study of the Southern Oscillation and Walker Circulation Phenomenon. American Meteorological Society, 0027-0644/78/1433-1451 Kajtar, J. B.; Santoso, A.; England, M. H.; Cai, W. 2017. Tropical climate variability interactions across the Pacific, Indian, and Atlantic Oceans. Climate Dynamics, Vol. 48, 2173-2190. DOI: 10.1007/s00382-016-3199-z Kayano, M. T.; Andreoli, R. V. 2006. Relationships between rainfall anomalies over northeastern Brazil and the El Nino-Southern Oscillation. Journal of Geophysical Research 111: D13102, DOI: 10.1029/2005JD006142 Kim, J.; Yu, J. 2021. Evolution of Subtropical Pacific-Onset El Niño: How Its Onset Location Controls Its Decay Evolution. Geophysical Research Letters Volume 48, Issue 5 e2020GL091345. https://doi.org/10.1029/2020GL091345 Larkin, N. K. e Harrison, D. E. 2005. Global seasonal temperature and precipitation anomalies during El Niño autumn and winter. Geophysical Research Letters, Vol. 32, L16705, DOI: 10.1029/2005GL022860 Latif, M.; Grotzner, A. 1999. The equatorial Atlantic oscillation and its response to ENSO. Climate Dynamics Vol. 16, 213-218. DOI: 10.1007/s003820050014 Lau, N.; Nath, M. J. 1996. The role of the “atmosphere bridge” in linking tropical Pacific ENSO events to extratropical SST anomalies. Journal of Climate 9:2036-2057 Lin, J; Qian, T. 2019. A New Picture of the Global Impacts of El Nino-Southern Oscillation. Scientific Reports 9, 17543. DOI: 10.1038/s41598-019-54090-5 Lockwood, J. G., 1984. The Southern Oscillation and El Niño. Progress in Physical Geography 1984 8: 102. DOI: 10.1177/030913338400800106 46 Losada, T.; Rodriguez-Fonseca, B.; Polo, I.; Janicot, S.; Gervois, S.; Chauvin, F.; Ruti, P. 2010. Tropical response to the Atlantic equatorial mode: AGCM multimodel approach. Climate Dynamics, DOI:10.1007/s00382-009-0624-6 Lubbecke, J. F.; Rodríguez-Fonseca, B; Richter, I.; Martín-Rey, M.; Losada, T.; Polo, I.; Keenlyside, N. S. 2018. Equatorial Atlantic variability – Modes, mechanisms, and global teleconnections. WIREs Climate Change, Vol. 9, Issue 4/e527. DOI: 10.1002/wcc.527 M. J. McPhaden. 1999. Genesis and evolution of the 1997–98 El Niño. Science, 283, pp. 950- 954. DOI: 10.1126/science.283.5404.950 Philander, S. G. H. 1983. El Niño Southern Oscillation phenomena. Nature 302, 295-301. DOI: 10.1038/302295a0 Philander, S. G. H., & Seigel, A. D. 1985. Chapter 33 Simulation of El Niño of 1982–1983. Elsevier Oceanography Series, 517–541. DOI:10.1016/s0422-9894(08)70729-3 Philander, S. G. 1999. El Nino: A Predictable Climate Fluctuation. National Forum 79.2: 11-4, ProQuest. Rao, V. B.; Hada, K., 1990. Characteristics of Rainfall over Brazil: Annual Variations and Connections with the Southern Oscillation. Theor. Appl. Climatol. 42, 81- 91. Rasmusson, E. M.; Carpenter, T. H. 1982. Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/El Nino. Monthly Weather Review 110: 354–384 Rodríguez-Fonseca, B.; Polo, I.; García-Serrano, J.; Losada, T.; Mohino, E.; Mechoso, C. R.; Kucharski, F. 2009. Are Atlantic Niños enhancing Pacific ENSO events in recent decades? Geophysical Research Letters, Vol. 36, L20705, DOI:10.1029/2009GL040048 Ropelewski, C. F.; Jones, P. D., 1987. An Extension of the Tahiti-Darwin Southern Oscillation Index. Monthly Weather Review, Vol. 115. 47 Schneider, Udo; Becker, Andreas; Finger, Peter; Meyer-Christoffer, Anja; Rudolf, Bruno; Ziese, Markus (2011): GPCC Full Data Reanalysis Version 6.0 at 1.0°: Monthly LandSurface Precipitation from Rain-Gauges built on GTS-based and Historic Data. DOI: 10.5676/DWD_GPCC/FD_M_V7_100 Schwing, F. B., Murphree, T., de Witt, L., & Green, P., 2002. The evolution of ocean and atmosphere anomalies in the Northeast Pacific during the El Niño and La Niña events of 1995–99. Progress in Oceanography, this issue. DOI: https://doi.org/10.1016/S0079- 6611(02)00064-2 H. Tokinaga, I. Richter, Y. Kosaka. 2019. ENSO Influence on the Atlantic Niño, Revisited: Multi-Year versus Single-Year ENSO Events. American Meteorological Society, Vol. 32, 4585-4600. DOI: 10.1175/JCLI-D-18-0683.1 Trenberth, K. E., 1976: Spatial and temporal variations of the Southern Oscillation. Quart. J. Roy. Meteor. Soc., 102,639-653 Trenberth, K. E., 1991: General characteristics of El Nino-Southern Oscillation. Teleconnections Linking Worldwide Climate Anomalies. M. Glantz, R. W. Katz, and N. Nicholls, Eds., Cambridge Univ. Press, 13-41. Trenberth, K. E. 1997. The Definition of El Niño. Bulletin of the American Meteorological Society, Vol. 78: Issue 12. DOI: https://doi.org/10.1175/1520- 0477(1997)078<2771:TDOENO>2.0.CO;2 Trenberth, K. E., 2013. El Niño – Southern Oscillation (ENSO). National Center for Atmospheric Research, Reference Module in Earth Systems and Environmental Sciences DOI:http://dx.doi.org/10.1016/B978-0-12-409548-9.04082-3 Troup, A. J., 1965. The ‘southern oscillation’. Division of Meteorological Physics, 551.513.7 : 551.543 : 519.27 48 Walker, G.; Bliss, E. World weather, iv. memo. r. Meteorol. Soc, v. 3, n. 24, p. 81–95, 1930. 19 Wang, C.; Deser, C.; Yu, J.; DiNezio, P.; Clement, A. 2016. El Niño and Southern Oscillation (ENSO): A Review. Coral Reefs of the World, Vol. 8. Springer, Dordrecht. DOI: 10.1007/978-94-017-7499-4_4 Wu, X.; Okumura, Y. M.; DiNezio, P. N. 2015. What Controls the Duration of El Niño and La Niña Events? American Meteorological Society, P5941–5965. DOI: 10.1175/JCLI-D-18- 0681.1 Zebiak, S. E. 1993. Air-Sea Interaction in the Equatorial Atlantic Region. Journal of Climate, Vol. 6: Issue 8, 1567-1586. DOI: 10.1175/1520-0442pt_BR
dc.subject.cnpqClimatologiapt_BR
dc.publisher.initialsUEApt_BR
Aparece nas coleções:EST - Trabalho de Conclusão de Curso Graduação

Arquivos associados a este item:
Arquivo Descrição TamanhoFormato 
Diferenças entre as evoluções temporais dos ENOS plurianuais e.pdf4,77 MBAdobe PDFVisualizar/Abrir


Os itens no repositório estão protegidos por copyright, com todos os direitos reservados, salvo quando é indicado o contrário.