ANALYSIS OF THE VERTICALLY INTEGRATED MOISTURE FLUX CONVERGENCE OVER BRAZIL PREDICTED BY WRF MODEL

Authors

  • Wiliam Morales Universidade Federal de Pelotas - UFPel
  • Yoshihiro Yamasaki Universidade Federal de Pelotas - UFPel

DOI:

https://doi.org/10.5902/2179460X17998

Keywords:

WRF, CFUVI, mesoescala, fluxo de umidade

Abstract

In the South America the regions of occurrence of the Low-Level-Jet at East Andes (LLJEA) and South Atlantic Convergence Zone (SACZ) where there are the largest import continental moisture. These two systems act over southern and southeast especially in the warm seasons of the year. Throughout 2011, the forecasts made by non-hydrostatic mesoscale Weather Research and Forecasting (WRF) model (SKAMAROCK et al., 2008) with 18 km grid spatial resolution and 35 vertical levels were used to analyze the Vertically Integrated Moisture Flux Convergence (VIMFC) fields and explore its relevance in the short-term forecasting activities. Several events of intense precipitation occurred during the 2011 year over Brazil were associated with LLJEA and SACZ, and two of them are presented. The results show meaning especially in their prediction with forecast horizon of 3 hours before the occurrence of storms. The study showed that the VIMFC prognosis indicated that there is a good agreement in terms of the location of cloudclusters that have been developed, compared with the corresponding representations in sequences compared with the of satellite images in the three hours after.

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Author Biographies

Wiliam Morales, Universidade Federal de Pelotas - UFPel

Departamento da Faculdade de Meteorologia

Yoshihiro Yamasaki, Universidade Federal de Pelotas - UFPel

Departamento da Faculdade de Meteorologia

References

AMARAL, L. M. C.; HOMANN, C. T.; YAMASAKI, Y. Sistema integrado IDD e modelo de mesoescala. In: VIII LATIN AMERICAN AND IBERIAN CONGRESS OF METEOROLOGY CLIMET XIII X CONGRESS OF METEOROLOGY CONGREMET X. 10., 2009, Buenos Áires. Anais…Buenos Áires, 2009.

ARAKAWA, A.; LAMB, V. R. Computational design of the basic dynamical processes of the UCLA general circulation model. General circulation models of the atmosphere. (A78-10662 01 – 47) New York: Academic Press, p.173-265, 1977.

ARRAUT, J. M.; SATYAMURTY, P. Precipitation and water vapor transport in the southern hemisphere with emphasis on the South American region. Journal of Applied Meteorology and Climatology, v.48, p.1902-1912, 2009.

BANACOS, P.; SCHULTZ, D. The use of moisture flux convergence in forecasting convective initiation: historical and operational perspectives. Weather and Forecast, v.20, n.3, p. 351-366, 2005.

BONNER, W. D. Climatology of the Low Level Jet. Monthly Weather Review, v.96, n.12, p.833-850, 1968.

CENTRO DE PREVISÃO DO TEMPO E ESTUDOS CLIMÁTICOS / INSTITUTO NACIONAL DE PESQUISAS ESPACIAIS. Disponível em: <http://tempo.cptec.inpe.br/> Acesso em: 12 jul. 2012.

DOUGLAS, M. W.; NICOLINI, M.; SAULO, A. C. The Low-Level jet at Santa Cruz, Bolívia during January-March 1998, pilot balloon observations and model comparisons. In: SYMPOSIUM ON GLOBAL CHANGE STUDIES, 10., 1999, Dallas. Anais … Dallas, 1999. p.223-226.

DUDHIA, J. Numerical Study of convection observed during the winter monsoon experiment using a mesoscale two-dimensional model. Journal of Atmospheric Sciences, v.46, n.20, p.3077-3107,1989.

HUDSON, H. On the ralationship between horizontal moisture convergence and convective cloud formation. Journal of Applicate Meteorology, vol. 10, p.755-762, Aug.1971.

KODAMA, Y. Large-scale common features of subtropical precipitation zones (the Baiu frontal zone, the SPCZ and the SACZ) Part I: Characteristics of subtropical frontal zones. Journal of the Meteorological Society of Japan, v.70, n.4, p.813-835, 1992.

KUO, H.L. On formation and intensification of tropical cyclones through latent heat release by cumulus convection. Journal of the Atmospheric Sciences, v.22, p.40-63, 1965.

KUO, H. L. Further studies of the parameterization of the influence of cumulus convection on large-scale flow. Journal of the Atmospheric Sciences, v.31, p.1232-1240, 1974.

LIEBMANN, B.; KILADIS, G. N.; VERA, C. S.; SAULO, A. C.; CARVALHO, L. M, V. Sub-seasonal variations of rainfall in south America in the vicinity of the Low-Level-Jet east of the Andes and comparison to those in the South Atlantic Convergence Zone. Journal of climate, v.17, n.19, p.3829-3842, 2004.

LIMA, K. C.; SATYAMURTY, P. Post-summer heavy rainfall events in Southeast Brazil associated with South Atlantic Convergence Zone. Atmospheric Science Letters, n.11, p.13-20, 2010.

MARENGO, J. A.; SOARES, W.R. Episódios de Jatos de Baixos Níveis ao Leste dos Andes durante 13-19 de abril de 1999. Revista Brasileira de Meteorologia, v.17, n.1, p.35-52, 2002.

MISRA, V.; DIRMEYER, P. A.; KIRTKMAN, B. P.; JUANG, H.; KANAMITSU, M. Regional simulation of Interannual Variability over South America. Journal of Geophysical Research, v.107, n.d20, p.8036-8051, 2002.

NOGUES-PAEGLE, J.; MO, K. C. Alternating wet and dry conditions over South America during summer. Monthly Weather Review, v.125, n.2, p.279-291, 1997.

PAEGLE, J. A comparative review of South American Low Level Jets. Meteorologica, v.3, n.1-2, p.73-81, 1998.

PEIXOTO, José Pinto; OORT, Abraham. Physics of Climate. 1.ed. New York: Springer, 1992. 520p.

PESQUEIRO, José Fernando. Balanço de umidade na região do sistema de monção da América do Sul em cenários climáticos futuros (2071-2100) utilizando o modelo Eta: um estudo de caso de modelagem. 2009. 242f. Tese (Doutorado em Meteorologia) – Instituto Nacional de Pesquisas Espaciais (INPE), São José dos Campos.

QUADRO, Mario Francisco Leal de. Estudo de episódios de Zona de Convergência do Atlântico Sul (ZCAS) sobre a América do sul. 1994. 99f. Dissertação (Mestrado em Meteorologia) - Instituto Nacional de Pesquisas Espaciais (INPE), São José dos Campos.

REBOITA, M. S.; GAN, M. A.; DA ROCHA, R. P.; AMBRIZZI, T. Regimes de precipitação na América do Sul: uma revisão bibliográfica. Revista Brasileira de Meteorologia, v.24, n.2, p.185-204, 2010.

SATYAMURTY, P.; DA COSTA, C.; DOS SANTOS, A. C.; MANZI, A. O. Convergência do fluxo de umidade sobre a região Amazônia nos anos contrastantes 2005 e 2009. In: XVI CONGRESSO BRASILEIRO DE METEOROLOGIA. 6., 2010. Belém. Anais … Belém, 2010.

SELUCHI, M. E.; MARENGO, J. A. Tropical-mid latitude exchange of air masses during Summer and Winter in South America: Climatic aspects and extreme events. International Journal of Climatology, v.20, n.10, p.1167-119, 2000.

SELUCHI, M. E.; SAULO, A. C. Baixa do Noroeste argentino e Baixa do Chaco: características,diferenças e semelhanças. Revista Brasileira de Meteorologia, v.27, n.1, p.49-60, 2012.

SKAMAROCK, W. C; KLEMP, J. B; DUDHIA, J. ; GILL, D. O; BARKER, D. M; WANG, W; POWERS, J. G. A Description of the Advanced Research WRF Version 3. NCAR/Tech. Notes, 2008.

SKAMAROCK, W.C; WEISMAN, M. L. The impact of positive-definitive moisture transport on NWP precipitation forecasts. Monthly weather review :submitted. 2008.

THE WEATHER RESEARCH & FORECASTING MODEL. Disponível em: <http://www.wrf-model.org/index.php> Acesso em: 05 abr. 2012.

UNIVERSITY OF WYOMING. Department of Atmospheric Science. Weather. Disponível em: <http://weather.uwyo.edu/> Acesso em: 13 ago. 2012.

VAN ZOMEREN, J; VAN DELDEN, A. Vertically integrated moisture flux convergence as a predictor of thunderstorms. Atmospheric and Research, v.83, n. 2-4, p. 435-445, 2007.

WALDSTREICHER, J. A guide to utilizing moisture flux convergence as a predictor of convection. National Weather Dig. Vol. 14, n. 4, p. 20-35, 1989.

WICKER, L. J; SKAMAROCK, W. C. Time splitting methods for elastic models using forward time schemes. Monthly weather review, n.130, p.2088-2097, 2002.

WRF (ARW) Version 3 Modeling System User's Guide. Mesoscale & Microscale Meteorology Division, National Center for Atmospheric Research, Boulder, Colorado, U.S.A., Jan. 2012. Disponível em: <http://www.mmm.ucar.edu./wrf/users/> Acesso em: 10 jun. 2012.

Published

2016-01-31

How to Cite

Morales, W., & Yamasaki, Y. (2016). ANALYSIS OF THE VERTICALLY INTEGRATED MOISTURE FLUX CONVERGENCE OVER BRAZIL PREDICTED BY WRF MODEL. Ciência E Natura, 38(1), 371–381. https://doi.org/10.5902/2179460X17998

Issue

Section

Meteorology