Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations

A mesoscale boundary-layer model is used to simulate low-level regional wind fields over the La Plata River of South America, a region characterized by a strong daily cycle of land–river surface-temperature contrast and low-level circulations of sea–land breeze type. The initial and boundary conditi...

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Autores principales: Berri, Guillermo Jorge, Bertossa, German
Formato: Articulo
Lenguaje:Inglés
Publicado: 2018
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/146251
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id I19-R120-10915-146251
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Geofísica
Boundary-layer model
Forecast errors
Initialization data
Low-level wind fields
Radiosonde observations
spellingShingle Geofísica
Boundary-layer model
Forecast errors
Initialization data
Low-level wind fields
Radiosonde observations
Berri, Guillermo Jorge
Bertossa, German
Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
topic_facet Geofísica
Boundary-layer model
Forecast errors
Initialization data
Low-level wind fields
Radiosonde observations
description A mesoscale boundary-layer model is used to simulate low-level regional wind fields over the La Plata River of South America, a region characterized by a strong daily cycle of land–river surface-temperature contrast and low-level circulations of sea–land breeze type. The initial and boundary conditions are defined from a limited number of local observations and the upper boundary condition is taken from the only radiosonde observations available in the region. The study considers 14 different upper boundary conditions defined from the radiosonde data at standard levels, significant levels, level of the inversion base and interpolated levels at fixed heights, all of them within the first 1500 m. The period of analysis is 1994–2008 during which eight daily observations from 13 weather stations of the region are used to validate the 24-h surface-wind forecast. The model errors are defined as the root-mean-square of relative error in wind-direction frequency distribution and mean wind speed per wind sector. Wind-direction errors are greater than wind-speed errors and show significant dispersion among the different upper boundary conditions, not present in wind speed, revealing a sensitivity to the initialization method. The wind-direction errors show a well-defined daily cycle, not evident in wind speed, with the minimum at noon and the maximum at dusk, but no systematic deterioration with time. The errors grow with the height of the upper boundary condition level, in particular wind direction, and double the errors obtained when the upper boundary condition is defined from the lower levels. The conclusion is that defining the model upper boundary condition from radiosonde data closer to the ground minimizes the low-level wind-field errors throughout the region.
format Articulo
Articulo
author Berri, Guillermo Jorge
Bertossa, German
author_facet Berri, Guillermo Jorge
Bertossa, German
author_sort Berri, Guillermo Jorge
title Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
title_short Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
title_full Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
title_fullStr Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
title_full_unstemmed Initializing a Mesoscale Boundary-Layer Model with Radiosonde Observations
title_sort initializing a mesoscale boundary-layer model with radiosonde observations
publishDate 2018
url http://sedici.unlp.edu.ar/handle/10915/146251
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