Zobrazeno 1 - 10
of 54
pro vyhledávání: '"Franciano Scremin Puhales"'
Autor:
Gustavo Rasera, Vagner Anabor, Luiz Angelo Steffenel, Damaris Kirsch Pinheiro, Franciano Scremin Puhales, Lissette Guzmán Rodríguez, Lucas Vaz Peres
Publikováno v:
Meteorological Applications, Vol 28, Iss 6, Pp n/a-n/a (2021)
Abstract During the southern spring, a break of the polar vortex over the Antarctic continent frequently occurs. This results in the advection of ozone‐poor air mass (O3) to mid‐latitudes, characterizing the secondary effect of the Antarctic ozon
Externí odkaz:
https://doaj.org/article/152416f79bec4061b538c13a5416553c
Autor:
Umberto Rizza, Elisa Canepa, Antonio Ricchi, Davide Bonaldo, Sandro Carniel, Mauro Morichetti, Giorgio Passerini, Laura Santiloni, Franciano Scremin Puhales, Mario Marcello Miglietta
Publikováno v:
Atmosphere, Vol 9, Iss 8, p 301 (2018)
Occasionally, storms that share many features with tropical cyclones, including the presence of a quasi-circular “eye” a warm core and strong winds, are observed in the Mediterranean. Generally, they are known as Medicanes, or tropical-like cyclo
Externí odkaz:
https://doaj.org/article/9aa94fbfe25c4c1394a45792c7add804
Autor:
Rafael Maroneze, Felipe Denardin Costa, Otávio Costa Acevedo, Luiz Eduardo Medeiros, Franciano Scremin Puhales, Vagner Anabor, Luca Mortarini
The present study introduces a new boundary layer parameterization for weather and forecasting models. It is implemented here as a boundary layer module in Weather Research and Forecasting (WRF) model. The main novelty in the new scheme is that it in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::371ece0a1b83ccf592836ce2323fb05c
https://doi.org/10.21203/rs.3.rs-2442980/v1
https://doi.org/10.21203/rs.3.rs-2442980/v1
Autor:
Rafael Maroneze, Felipe D'Almeida Costa, Franciano Scremin Puhales, Otávio C. Acevedo, Pablo E. S. Oliveira, Arlindo D. Carvalho
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 147:2335-2351
Autor:
Pablo E. S. Oliveira, Gervásio Annes Degrazia, Luis Gustavo Nogueira Martins, Otávio C. Acevedo, Franciano Scremin Puhales
Publikováno v:
Boundary-Layer Meteorology. 179:423-446
The correct simulation of pollutant dispersion in coastal regions demands understanding the turbulence structure of the thermal internal boundary layer (TIBL), which typically occurs in daytime when maritime air is advected over the continent. Such a
Autor:
Luiz Eduardo Medeiros, Luis Fernando Camponogara, Felipe D'Almeida Costa, Luca Mortarini, Rafael Maroneze, Franciano Scremin Puhales, Arlindo D. Carvalho, Otávio C. Acevedo, Daniel Michelon dos Santos
Publikováno v:
Journal of the Atmospheric Sciences. 77:2039-2054
Two contrasting flow regimes exist in the stable boundary layer (SBL), as evidenced from both observational and modeling studies. In general, numerical schemes such as those used in numerical weather prediction and climate models (NWPCs) reproduce a
Autor:
Giuliano Demarco, Luis Gustavo Nogueira Martins, Bardo Ernst Josef Bodmann, Franciano Scremin Puhales, Otávio Costa Acevedo, Adrian Roberto Wittwer, Felipe Denardin Costa, Debora Regina Roberti, Acir Mércio Loredo-Souza, Franco Caldas Degrazia, Tiziano Tirabassi, Gervásio Annes Degrazia
Publikováno v:
International Journal of Environmental Research and Public Health; Volume 19; Issue 9; Pages: 5134
The aim of this paper is to analyse the thermal effects in a wind tunnel experiment to simulate the planetary boundary layer (PBL). Experiments were performed in the wind tunnel of the Laboratory of Constructions Aerodynamics at the Federal Universit
Autor:
Lucas Vaz Peres, Gustavo Rasera, Luiz Angelo Steffenel, Lissette Guzmán Rodríguez, Damaris Kirsch Pinheiro, Vagner Anabor, Franciano Scremin Puhales
Publikováno v:
Meteorological Applications
Meteorological Applications, Wiley, 2021, 28 (6), ⟨10.1002/met.2034⟩
Meteorological Applications, Vol 28, Iss 6, Pp n/a-n/a (2021)
Meteorological Applications, Wiley, 2021, 28 (6), ⟨10.1002/met.2034⟩
Meteorological Applications, Vol 28, Iss 6, Pp n/a-n/a (2021)
International audience; During the southern spring, a break of the polar vortex over the Antarctic continent frequently occurs. This results in the advection of ozone-poor air mass (O3) to mid-latitudes, characterizing the secondary effect of the Ant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::01b64d3bd55c8580be7baa2a6d7ba421
https://hal.univ-reims.fr/hal-03462093
https://hal.univ-reims.fr/hal-03462093
Autor:
Felipe D'Almeida Costa, Rafael Maroneze, Giuliano Demarco, Otávio C. Acevedo, Luca Mortarini, Franciano Scremin Puhales
Publikováno v:
Quarterly Journal of the Royal Meteorological Society (2019). doi:10.1002/qj.3643
info:cnr-pdr/source/autori:Maroneze, Rafael; Acevedo, Otávio C.; Costa, Felipe D.; Puhales, Franciano S.; Demarco, Giuliano; Mortarini, Luca/titolo:The nocturnal boundary layer transition from weakly to very stable. Part II: Numerical simulation with a second-order model/doi:10.1002%2Fqj.3643/rivista:Quarterly Journal of the Royal Meteorological Society/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume
info:cnr-pdr/source/autori:Maroneze, Rafael; Acevedo, Otávio C.; Costa, Felipe D.; Puhales, Franciano S.; Demarco, Giuliano; Mortarini, Luca/titolo:The nocturnal boundary layer transition from weakly to very stable. Part II: Numerical simulation with a second-order model/doi:10.1002%2Fqj.3643/rivista:Quarterly Journal of the Royal Meteorological Society/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume
Observations of the vertical and temporal structure of the nocturnal boundary layer before and after a transition from the weakly to the very stable regime have been presented in Part I. Here, similar transitions are investigated using a one-dimensio
Autor:
Jônatan Dupont Tatsch, Daiane de Vargas Brondani, Otávio C. Acevedo, Franciano Scremin Puhales
Publikováno v:
Boundary-Layer Meteorology. 171:271-288
A new boundary-layer method is proposed to estimate sensible and latent heat fluxes on a monthly scale, based on hourly surface observations of temperature and specific humidity, as well as their vertical profile in the morning. It assumes that advec