4.7 Article

Toward Data-Driven Weather and Climate Forecasting: Approximating a Simple General Circulation Model With Deep Learning

期刊

GEOPHYSICAL RESEARCH LETTERS
卷 45, 期 22, 页码 12616-12622

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2018GL080704

关键词

machine learning; weather prediction; neural networks; deep learning; climate models

资金

  1. Department of Meteorology of Stockholm University
  2. Vetenskapsradet grant [2016-03724]
  3. Vinnova [2016-03724] Funding Source: Vinnova
  4. Swedish Research Council [2016-03724] Funding Source: Swedish Research Council

向作者/读者索取更多资源

It is shown that it is possible to emulate the dynamics of a simple general circulation model with a deep neural network. After being trained on the model, the network can predict the complete model state several time steps aheadwhich conceptually is making weather forecasts in the model world. Additionally, after being initialized with an arbitrary model state, the network can through repeatedly feeding back its predictions into its inputs create a climate run, which has similar climate statistics to the climate of the general circulation model. This network climate run shows no long-term drift, even though no conservation properties were explicitly designed into the network. Plain Language Summary Numerical weather prediction and climate models are complex computer programs that represent the physics of the atmosphere. They are essential tools for predicting the weather and for studying the Earth's climate. Recently, a lot of progress has been made in machine learning methods. These are data-driven algorithms that learn from existing data. We show that it is possible that such an algorithm learns the dynamics of a simple climate model. After being presented with enough data from the climate model, the network can successfully predict the time evolution of the model's state, thus replacing the dynamics of the model. This finding is an important step toward purely data-driven weather forecastingthus weather forecasting without the use of traditional numerical models and also opens up new possibilities for climate modeling.

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