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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Sociedade Brasileira de Meteorologia
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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. |
first_indexed | 2024-04-13T09:56:36Z |
format | Article |
id | doaj.art-65eb7fb1f08e4258b0cabbba251132b1 |
institution | Directory Open Access Journal |
issn | 1982-4351 |
language | English |
last_indexed | 2024-04-13T09:56:36Z |
publisher | Sociedade Brasileira de Meteorologia |
record_format | Article |
series | Revista Brasileira de Meteorologia |
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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