Development of novel hybrid machine learning models for monthly thunderstorm frequency prediction over Bangladesh
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Citations
Changes in monsoon precipitation patterns over Bangladesh and its teleconnections with global climate
Effects of convective available potential energy, temperature and humidity on the variability of thunderstorm frequency over Bangladesh
References
Random Forests
The Nature of Statistical Learning Theory
Statistical learning theory
Time series analysis, forecasting and control
The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis
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A SVR–ANN combined model based on ensemble EMD for rainfall prediction
Frequently Asked Questions (14)
Q2. Why is the winter season the least favorable for TSF?
The authors anticipate that due to low surface temperature and soil moisture, the 424 winter season (November to February) is the least favorable for forming TSF.
Q3. What are the main factors affecting the performance of the hybrid 496 models?
494 Second, the coupling preprocessing technique with a machine learning algorithm, a division of the training and 495 testing datasets, and model selection criteria are a vital factor affecting the overall performance of the hybrid 496 models.
Q4. Why is the frequency of severe thunderstorms likely to increase in the 21st century?
Severe thunderstorms frequency is likely to increase in the 21st century due to the 51 increasing convective instability (Rädler et al., 2019).
Q5. What are the contours of the simulated eld?
The deep cyan contours represent the Pearson correlation coe cient, green contours represent centered RMS error in the simulated eld, and violet contours represent the Standard Deviation of the simulated pattern.
Q6. What is the reason for the improved performance of EEMD-ANN?
One probable reason for the improved performance of 434 EEMD-ANN can be the method's capability to solve complex and nonlinear problems (Phuong et al., 2017).
Q7. What are the sensitive parameters for predicting LTSF?
Although the parameters like 404DP, KI, RH, ST, and WS50 have low sensitivity value, they help achieve better prediction accuracy.
Q8. What is the significance of the proposed methodology?
It can be said that the proposed methodology can not only predict the 456 complicated thunderstorm frequency over Bangladesh rationally well, but it can also attain extreme climatic 457 events.
Q9. What are the other parameters that have positively contributed to the model building?
All the other convective parameters, e.g., TT, CPRCP, CRR, KI, and the meteorological 477 parameters, e.g., PRCP, RH, ST, WS50, have positively contributed to the best model building.
Q10. What is the effect of the low SST and northeast wind flow on the TSF?
422 Uncertainty increases in low TSF months (winter) because of the low SST and northeast wind flow from the 423 BoB and lowers vapor flux availability.
Q11. How many IMFs are added to the same raw series?
Since the mean value of Gaussian white noise is equal to zero, the IMFs obtained are integrated and averaged 258 as the final result: 259 𝐼𝑀𝐹̅̅ ̅̅ ̅̅ = 1𝑁 ∑ 𝐶𝑗,𝑚𝑁𝑚=1 260 where 𝐶𝑗,𝑚 represents the 𝑗𝑡ℎ IMFs from the 𝑚𝑡ℎ time, 𝑁 denotes the number of the added white noise 261 sequences.
Q12. What is the main advantage of using EEMD in predicting severe events?
The application of machine learning algorithms in a 488 thunderstorm prediction brings with a new promise for forthcoming studies concerning both operational 489 predictors and meteorological research that intend to examine observed and future variations in frequencies of 490 severe extreme events (Yasen et al., 2017; Taszarek et al., 2019).
Q13. What is the main reason why the TSF prediction has received little attention in the literature?
100 However, TSF prediction has received little attention in the existing literature due to its complicated nature and 101 unique weather feature with high instability, making it difficult to predict.
Q14. What is the common approach used to predict thunderstorms?
Most of the studies have focused on Numerical Weather Prediction 82 (NWP) modeling or forecasting of a single thunderstorm event on an hourly basis based on the convective 83 indices.