Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region

Abstract In the present study, the physical parameterizations of the Weather Research and Forecasting (WRF) model are verified for making accurate inferences about the dynamics of the Thermal Internal Boundary Layer (TIBL) generated by sea breeze in an urban center with an island in a bay along a co...

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Main Authors: Nadir Salvador, Ayres G. Loriato, Alexandre Santiago, Taciana T.A. Albuquerque, Neyval C. Reis Jr., Jane M. Santos, Eduardo Landulfo, Gregori Moreira, Fábio Lopes, Gerhard Held, Davidson M. Moreira
Format: Article
Language:English
Published: Sociedade Brasileira de Meteorologia
Series:Revista Brasileira de Meteorologia
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862016000500593&lng=en&tlng=en
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author Nadir Salvador
Ayres G. Loriato
Alexandre Santiago
Taciana T.A. Albuquerque
Neyval C. Reis Jr.
Jane M. Santos
Eduardo Landulfo
Gregori Moreira
Fábio Lopes
Gerhard Held
Davidson M. Moreira
author_facet Nadir Salvador
Ayres G. Loriato
Alexandre Santiago
Taciana T.A. Albuquerque
Neyval C. Reis Jr.
Jane M. Santos
Eduardo Landulfo
Gregori Moreira
Fábio Lopes
Gerhard Held
Davidson M. Moreira
author_sort Nadir Salvador
collection DOAJ
description Abstract In the present study, the physical parameterizations of the Weather Research and Forecasting (WRF) model are verified for making accurate inferences about the dynamics of the Thermal Internal Boundary Layer (TIBL) generated by sea breeze in an urban center with an island in a bay along a coastal region with rugged topography. The simulations were performed using parameterizations from Yonsei University (YSU), Mellor-Yamada-Janjic (MYJ) and Asymmetric Convective Model version 2 (ACM2) for the atmospheric boundary layer (ABL) and Noah and Rapid Update Cycle (RUC) for the Land Surface Model (LSM). The data inferred by the WRF model were compared with those obtained by a Surface Meteorological Station (SMS) and by measurements generated using Light Detection and Ranging (LIDAR), Sonic Detection and Ranging (SODAR) and radiosonde. The simulations showed that although the object of this research was a region with high geographical complexity, the YSU parameterization set (non-local closure) for the ABL and the Noah parameterization for the LSM presented satisfactory results in determining ABL height generated by the sea breeze on the day in question.
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spelling doaj.art-65eb7fb1f08e4258b0cabbba251132b12022-12-22T02:51:22ZengSociedade Brasileira de MeteorologiaRevista Brasileira de Meteorologia1982-4351314 suppl 159360910.1590/0102-7786312314b20150093S0102-77862016000500593Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória RegionNadir SalvadorAyres G. LoriatoAlexandre SantiagoTaciana T.A. AlbuquerqueNeyval C. Reis Jr.Jane M. SantosEduardo LandulfoGregori MoreiraFábio LopesGerhard HeldDavidson M. MoreiraAbstract In the present study, the physical parameterizations of the Weather Research and Forecasting (WRF) model are verified for making accurate inferences about the dynamics of the Thermal Internal Boundary Layer (TIBL) generated by sea breeze in an urban center with an island in a bay along a coastal region with rugged topography. The simulations were performed using parameterizations from Yonsei University (YSU), Mellor-Yamada-Janjic (MYJ) and Asymmetric Convective Model version 2 (ACM2) for the atmospheric boundary layer (ABL) and Noah and Rapid Update Cycle (RUC) for the Land Surface Model (LSM). The data inferred by the WRF model were compared with those obtained by a Surface Meteorological Station (SMS) and by measurements generated using Light Detection and Ranging (LIDAR), Sonic Detection and Ranging (SODAR) and radiosonde. The simulations showed that although the object of this research was a region with high geographical complexity, the YSU parameterization set (non-local closure) for the ABL and the Noah parameterization for the LSM presented satisfactory results in determining ABL height generated by the sea breeze on the day in question.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862016000500593&lng=en&tlng=enbrisa marítimaWRFLIDARSODARparametrizaçãocamada limite interna térmica
spellingShingle Nadir Salvador
Ayres G. Loriato
Alexandre Santiago
Taciana T.A. Albuquerque
Neyval C. Reis Jr.
Jane M. Santos
Eduardo Landulfo
Gregori Moreira
Fábio Lopes
Gerhard Held
Davidson M. Moreira
Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
Revista Brasileira de Meteorologia
brisa marítima
WRF
LIDAR
SODAR
parametrização
camada limite interna térmica
title Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
title_full Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
title_fullStr Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
title_full_unstemmed Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
title_short Study of the Thermal Internal Boundary Layer in Sea Breeze Conditions Using Different Parameterizations: Application of the WRF Model in the Greater Vitória Region
title_sort study of the thermal internal boundary layer in sea breeze conditions using different parameterizations application of the wrf model in the greater vitoria region
topic brisa marítima
WRF
LIDAR
SODAR
parametrização
camada limite interna térmica
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862016000500593&lng=en&tlng=en
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