An Artificial Intelligence-Based Enso Diversity Prediction Method
An artificial intelligence and diversity technology, applied in weather forecasting, instruments, calculation models, etc., can solve the problem that the spatial type of El Niño is not well resolved, the forecasting ability of the Central Pacific type El Niño is not high, and the spatial diversity cannot be displayed and other issues to achieve the effect of reducing personnel and property losses, improving forecasting skills, and breaking through forecasting bottlenecks
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Embodiment 1
[0023] This embodiment provides an artificial intelligence-based ENSO diversity prediction method, such as figure 1 shown, including the following steps:
[0024] S1. Using the EOF decomposition method, the first three main modes are extracted from the observational data of sea surface temperature anomalies in the equatorial Pacific: zonally consistent, zonally inconsistent and central warming;
[0025] S2. Project the CMIP6 historical simulation data on the three main modes EOF main modes, and obtain three sets of historical simulation data PC values respectively;
[0026] S3. Use three sets of historical simulated data PC values as forecast values, use the SSTA of the initial month and the two sea temperature data of the Tendency item as the input values for training, and use the CMIP6 mode to train the improved deep learning model (VGG-11).
[0027] S4. Input the new observation data as the forecast input value into the trained model, including the abnormal value of ...
Embodiment 2
[0038] This example provides an El Niño forecasting process in the central Pacific El Niño-type occurrence region using the data on the surface of the equatorial Pacific Ocean from 1984 to 2017.
[0039] In this example, the warm pool index (WPI) is used to evaluate and compare the forecast results of the Central Pacific El Niño.
[0040] 1. Use EOF to decompose the observed equatorial Pacific SSTA data to obtain the first three main modes (EOF1-3, such as figure 2 )
[0041] 2. Projecting the SSTA of 39 CMIP6 historical patterns (time: 1948–2014) into the three EOF main modalities, the PC values for each month from 1948 to 2014 can be obtained; at the same time, it can be obtained from the 39 historical patterns SSTA and Tendency items for each month.
[0042] 3. Use the SSTA and Tendency of the initial month to input the deep learning model, and output the 3 PC values predicted N months in advance (N=1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11); Since there are a large amount ...
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