Daniela Buske

Dr. Daniela Buske

orcid

Research Focus & Metrics

Academic Career Length

22Years (2005-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 April 2005 in Atmospheric Environment
Verified
Journal Article
Closed access
SWS. Wortmann
S. Wortmann
MVM.T. Vilhena
M.T. Vilhena
DMDavidson Martins Moreira
Davidson Martins Moreira
DBDaniela Buske
Daniela Buske

1 March 2009 in Atmospheric Research
Verified
Journal Article
Closed access
DMDavidson Martins Moreira
Davidson Martins Moreira
MVM.T. Vilhena
M.T. Vilhena
DBDaniela Buske
Daniela Buske
TTTiziano Tirabassi
Tiziano Tirabassi

1 November 2005 in Atmospheric Environment
Verified
Journal Article
Closed access
DMDavidson Martins Moreira
Davidson Martins Moreira
MVM.T. Vilhena
M.T. Vilhena
TTTiziano Tirabassi
Tiziano Tirabassi
DBDaniela Buske
Daniela Buske
Renato CottaRenato Cotta
Renato Cotta

23 March 2006 in Atmospheric Environment
Verified
Journal Article
Closed access
DMDavidson Martins Moreira
Davidson Martins Moreira
MVM.T. Vilhena
M.T. Vilhena
DBDaniela Buske
Daniela Buske
TTTiziano Tirabassi
Tiziano Tirabassi

1 August 2007 in Atmospheric Environment
Verified
Journal Article
Closed access
DBDaniela Buske
Daniela Buske
MVMarco T. Vilhena
Marco T. Vilhena
DMDavidson Martins Moreira
Davidson Martins Moreira
TTTiziano Tirabassi
Tiziano Tirabassi

1 August 2008 in Journal of Applied Meteorology and Climatology
Verified
Journal Article
Open access
TTTiziano Tirabassi
Tiziano Tirabassi
DBDaniela Buske
Daniela Buske
DMDavidson Martins Moreira
Davidson Martins Moreira
MVMarco T. Vilhena
Marco T. Vilhena
A mathematical scheme is developed to simulate the vertical turbulent dispersion of air pollution that is absorbed or deposited to the ground. The scheme is an exact analytical solution of the atmospheric diffusion equation, without any restriction to the vertical profile of wind speed and eddy diffusivities, and taking into account the dry deposition by a boundary condition of a nonzero flux to the ground. The performances of the solution, with a proper parameterization of the vertical profiles of the wind and eddy diffusivities, were evaluated against the dataset from the Hanford (Washington) diffusion experiment, in which two tracers (one depositing and one nondepositing) were released simultaneously. In addition, the solution derived in this work is compared with four different models, with deposition at the ground, found in the literature.