2016
DOI: 10.5540/03.2016.004.01.0097
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Artificial Neural Networks emulating Representer Method at a shallow water model 2D

Abstract: Abstract. The goal of the present work is to employ artificial neural networks as a data assimilation method applied to shallow water equation. This model is used to represent ocean dynamics. Data assimilation is a computational procedure to combine observation data with model data for identifying the best initial condition (analysis) to an operational prediction system. Here we compare two techniques: representer method and artificial neural network.

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Cited by 3 publications
(3 citation statements)
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“…The machine learning methods for DA are summarized in Table 5. Wave model [111] MLP PF Lorenz model [120] MLP KF Three-wave model [121] MLP Variational Lorenz model [122] MLP Variational Wave model [107] Elman KF Shallow water 1D model (DYNAMO-1D) [104] RBF KF Shallow water 1D model (DYNAMO-1D) [112] MLP LETKF Atmospheric general circulation model (FSUGSM) [123] MLP LETKF Atmospheric general circulation model (SPEEDY) [124] Mixed Type KF Satellite-Derived Sea Surface Temperature data [125] Fully Connected Variational , KF Dot system and Lorenz models [117] LSTM Variational (3DVAR) CFD model (Fluidity) [114] Elman Variational Dot system and Lorenz models [102] LSTM KF CFD model (Fluidity) [101] MLP Variational Lorenz model [126] LSTM Variational Lorenz model [127] MLP Variational and EnKF Lorenz model [118] LSTM KF Oxygen diffusion across the Blood-Brain Barrier model…”
mentioning
confidence: 99%
“…The machine learning methods for DA are summarized in Table 5. Wave model [111] MLP PF Lorenz model [120] MLP KF Three-wave model [121] MLP Variational Lorenz model [122] MLP Variational Wave model [107] Elman KF Shallow water 1D model (DYNAMO-1D) [104] RBF KF Shallow water 1D model (DYNAMO-1D) [112] MLP LETKF Atmospheric general circulation model (FSUGSM) [123] MLP LETKF Atmospheric general circulation model (SPEEDY) [124] Mixed Type KF Satellite-Derived Sea Surface Temperature data [125] Fully Connected Variational , KF Dot system and Lorenz models [117] LSTM Variational (3DVAR) CFD model (Fluidity) [114] Elman Variational Dot system and Lorenz models [102] LSTM KF CFD model (Fluidity) [101] MLP Variational Lorenz model [126] LSTM Variational Lorenz model [127] MLP Variational and EnKF Lorenz model [118] LSTM KF Oxygen diffusion across the Blood-Brain Barrier model…”
mentioning
confidence: 99%
“…Como aponta a cartela da Amérique méridionale, 3 o viajante francês Charles Marie de La Condamine desempenhou importante papel na configuração espacial que D'Anville imprimiu à região da bacia Amazônica, mesmo em trechos, como o rio Negro, que jamais visitou. 4 La Condamine, juntamente com Pierre Bouguer, sob a direção de Louis Godin, integrou, em 1735, a expedição espano-francesa que foi ao Peru medir um arco de meridiano, no contexto do debate sobre o formato da terra. 5 Ao fim da expedição, ele decidiu retornar à Europa descendo o Amazonas, o que fez entre maio e setembro de 1743, pois o trajeto do rio era de grande interesse entre os savants europeus, já que seu conhecimento era, até então, bastante relativo.…”
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“…[13] applied NN to emulate the particle filter and the variational data assimilation (4D var) for the Lorenz chaotic system. In 2012, Furtado [40] used an ocean model to emulate a variational method called representer. The NN technique was successful for all experiments, but they use theoretical or low-dimensional models.…”
Section: Introductionmentioning
confidence: 99%