Buscar
Mostrando ítems 1-10 de 596
Impact of climate change on monthly streamflow in the Verde River Basin using two hydrological modelsImpactos das mudanças climáticas na vazão mensal da bacia do Rio Verde usando dois modelos hidrológicos
(Instituto de Pesquisas Ambientais em Bacias Hidrográficas (IPABHi), 2022)
Evaluation of Eta Model Rainfall Forecasts at São Francisco River Basin in Minas Gerais, BrazilAvaliação das Previsões de Precipitação do Modelo Eta para Bacia do Rio São Francisco em Minas Gerais, Brasil
(Centro de Ciências Matemáticas e da Natureza, Instituto de Geociências, Universidade Feder, 2016)
Maximum Likelihood Estimator For The Alpha-eta-mu Fading Environment
(IEEENew York, 2016)
MID-HOLOCENE CLIMATE SIMULATIONS OVER BRAZIL USING THE ETA REGIONAL PALEOCLIMATE MODELSIMULAÇÕES CLIMÁTICAS DO HOLOCENO MÉDIO PARA O BRASIL UTILIZANDO O MODELO REGIONAL PALEOCLIMÁTICO ETA
(Instituto de Pesquisas Ambientais, Secretaria de Infraestrutura e Meio Ambiente/SP, 2023)
Constraining the orbital orientation of eta Carinae from H Paschen lines
(WILEY-BLACKWELL, 2009)
During the past decade, several observational and theoretical works have provided evidence of the binary nature of eta Carinae. Nevertheless, there is still no direct determination of the orbital parameters, and the different ...
The eta-mu joint phase-envelope distribution
(Ieee-inst Electrical Electronics Engineers IncPiscatawayEUA, 2007)
Estimativa da evapotranspiração real via sensoriamento remoto
(Universidade Federal de Minas GeraisBrasilENG - DEPARTAMENTO DE ENGENHARIA SANITÁRIA E AMBIENTALPrograma de Pós-Graduação em Saneamento, Meio Ambiente e Recursos HídricosUFMG, 2018-09-28)
Actual evapotranspiration (ETa) is one of the main hydrological cycle processes and the main cause of surface water loss. The precise knowledge of ETa rates along time and space is necessary for modeling water balance in ...
Revisiting 2D numerical models for the 19th century outbursts of eta Carinae
(WILEY-BLACKWELL, 2010)
We present here new results of two-dimensional hydrodynamical simulations of the eruptive events of the 1840s (the great) and the 1890s (the minor) eruptions suffered by the massive star eta Carinae (Car). The two bipolar ...