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Geração de VRS a partir de modelos atmosféricos: Conceito, implementação e resultados
(2007-07-01)
Nowadays, with the implantation of GNSS (Global Navigation Satellite System) reference station networks, several positioning techniques have been developed and/or improved. Using such kind of network data it is possible ...
Geração de VRS a partir de modelos atmosféricos: Conceito, implementação e resultados
(2007-07-01)
Nowadays, with the implantation of GNSS (Global Navigation Satellite System) reference station networks, several positioning techniques have been developed and/or improved. Using such kind of network data it is possible ...
A numerical investigation of the atmosphere-ocean thermal contrast over the coastal upwelling region of Cabo Frio, Brazil
(CENTRO CIENCIAS ATMOSFERA UNAM, 2008)
An one-dimensional atmospheric second order closure model, coupled to an oceanic mixed layer model, is used to investigate the short term variation of the atmospheric and oceanic boundary layers in the coastal upwelling ...
Land surface atmosphere interaction in future South American climate using a multi-model ensemble
(Wiley, 2015-12)
The land-atmosphere interaction for reference and future climate is estimated with a regional climate model ensemble. In reference climate, more than 50% of the models show interaction in southeastern South America during ...
Characterization of the atmospheric depth profile using the ground-level temperature: The case of Malargüe, Argentina
(Springer Heidelberg, 2013-09)
We present a study of the atmospheric depth profile and the dependence with its characteristic parameters. We introduce a new model, named GAMMA, based on a parameterization that allows us to obtain the atmospheric depth ...
Impacts of eCO2 vs. deforestation on Amazon climate modelled with the CPTEC-BAM
(Repositório de Dados de Pesquisa da Unicamp, 2021)
Land-Atmosphere Coupling Sensitivity to GCMs Resolution: A Multimodel Assessment of Local and Remote Processes in the Sahel Hot Spot
(Amer Meteorological Soc, 2020-11)
Land–atmosphere interactions are often interpreted as local effects, whereby the soil state drives local atmospheric conditions and feedbacks originate. However, nonlocal mechanisms can significantly modulate land–atmosphere ...