EVALUATION OF DIFFERENT BOUNDARY LAYER SCHEMES FOR FOG EVENTS SIMULATION AND FORECASTING IN RIO GRANDE DO SUL

Authors

  • Nórton Franciscatto de Paula Programa de Pós-Graduação em Meteorologia da UFSM/GruMA
  • Franciano Scremin Puhales Departamento de Física da UFSM/GruMA
  • Gabriele Golart Silva Curso de Graduação em Meteorologia da UFSM/GruMA
  • Jéssica Melo Mintegui Programa de Pós-Graduação em Meteorologia da UFSM/GruMA
  • Vagner Anabor Departamento de Física da UFSM/GruMA
  • Everson Dal Piva Departamento de Física da UFSM/GruMA
  • Felipe Denardin Costa Universidade Federal do Pampa

DOI:

https://doi.org/10.5902/2179460X25940

Keywords:

Fog, WRF, Planetary Boundary Layer, Mellor-Yamada-Janic (MYJ), Yonsei University (YSU)

Abstract

In this work we used two boundary layer schemes to reproduce numerically a persistent fog event in Santa Maria, Rio Grande do Sul. The model employed was WRF using, as initial and boundary conditions, GFS data. The boundary layer employed schemes were the Mellor-Yamada-Janic (MYJ) and Yonsei University (YSU). Generally, boundary layer overestimate of wind speed values schemes 10m and represent relatively well temperature. However, the relative humidity does not represent the fog condition, not reaching saturation in some cases. When saturation is achieved the same if not properly maintained during the occurrence of the event.

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Author Biographies

Nórton Franciscatto de Paula, Programa de Pós-Graduação em Meteorologia da UFSM/GruMA

Franciano Scremin Puhales, Departamento de Física da UFSM/GruMA

Gabriele Golart Silva, Curso de Graduação em Meteorologia da UFSM/GruMA

Jéssica Melo Mintegui, Programa de Pós-Graduação em Meteorologia da UFSM/GruMA

Vagner Anabor, Departamento de Física da UFSM/GruMA

Everson Dal Piva, Departamento de Física da UFSM/GruMA

Felipe Denardin Costa, Universidade Federal do Pampa

References

HONG, S. Y., NOH, Y., DUDHIA, J. (2006). A new vertical diffusion package with an explicit treatment of entrainment processes. Monthly Weather Review, 134(9), 2318–2341.

JANJIC, Z. I. (1994). The step-mountain eta coordinate model: Further evelopments of the convection, viscous sublayer, and turbulence closure schemes. Monthly Weather Review, 122(5), 927–945.

NCEP (2000). National centers for environmental prediction/national weather service/"NOAA". URL http://www.emc.ncep.noaa.gov/index.php?branch=GFS,acessado em 22 set 2014.

DE PAULA, N. F., PUHALES, F. S., ANABOR, V., PIVA, E. D., DE LIMA NASCIMENTO, E. (2015). Características meteorológicas médias associadas a nevoeiro de radiação em santa maria – rs. Ciência e Natura, 37(3), 613–624.

SKAMAROCK, W. C., KLEMP, J. B., DUDHIA, J., GILL, D. O., BARKER, D. M., DUDA, M. G., HUANG, X. Y., WANG, W., POWERS, J. G. (2008). A Description of the Advanced Research WRF Version 3. Boulder, URL http://www2.mmm.ucar.edu/wrf/users/docs/arw_v3.pdf.

XIE, B., FUNG, J. C., CHAN, A., LAU, A. (2012). Evaluation of nonlocal and local planetary boundary layer schemes in the wrf model. Journal of Geophysical Research, 117(D12103).

Published

2017-05-23

How to Cite

Paula, N. F. de, Puhales, F. S., Silva, G. G., Mintegui, J. M., Anabor, V., Piva, E. D., & Costa, F. D. (2017). EVALUATION OF DIFFERENT BOUNDARY LAYER SCHEMES FOR FOG EVENTS SIMULATION AND FORECASTING IN RIO GRANDE DO SUL. Ciência E Natura, 39(2), 451–458. https://doi.org/10.5902/2179460X25940

Issue

Section

Meteorology

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