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Medium-range forecast of cyclogenesis over North Indian Ocean with multilayer perceptron model using satellite data

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Abstract

An attempt is made in this study to develop a model to forecast the cyclonic depressions leading to cyclonic storms over North Indian Ocean (NIO) with 3 days lead time. A multilayer perceptron (MLP) model is developed for the purpose and the forecast quality of the model is compared with other neural network and multiple linear regression models to assess the forecast skill and performances of the MLP model. The input matrix of the model is prepared with the data of cloud coverage, cloud top temperature, cloud top pressure, cloud optical depth, cloud water path collected from remotely sensed moderate resolution imaging spectro-radiometer (MODIS), and sea surface temperature. The input data are collected 3 days before the cyclogenesis over NIO. The target output is the central pressure, pressure drop, wind speed, and sea surface temperature associated with cyclogenesis over NIO. The models are trained with the data and records from 1998 to 2008. The result of the study reveals that the forecast error with MLP model varies between 0 and 7.2 % for target outputs. The errors with MLP are less than radial basis function network, generalized regression neural network, linear neural network where the errors vary between 0 and 8.4 %, 0.3 and 24.8 %, and 0.3 and 32.4 %, respectively. The forecast with conventional statistical multiple linear regression model, on the other hand, generates error values between 15.9 and 32.4 %. The performances of the models are validated for the cyclonic storms of 2009, 2010, and 2011. The forecast errors with MLP model during validation are also observed to be minimum.

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References

  • Bhalme HN (1972) Trends and quasi-biennial oscillation in the series of cyclonic disturbances over the Indian region. Indian J Meteorol Geophys 23(3):355–358

    Google Scholar 

  • Bodri L, Cermak V (2000) Prediction of extreme precipitation using a neural network: application to summer flood occurrence in Moravia. Adv Eng Softw 31:311–321

    Article  Google Scholar 

  • Bose NK, Liang P (1995) Neural Network Fundamentals with Graphs, algorithms and applications, McGraw Hill, I edn. The MIT Press, Bambridge

    Google Scholar 

  • Chaudhuri S (2006) A hybrid model to estimate the depth of potential convective instability during severe thunderstorms. Soft Comput Fusion Found Methodol Appl 10:243–248

    Google Scholar 

  • Chaudhuri S (2010) Convective energies in forecasting severe thunderstorms with one hidden layer neural net and variable learning rate back propagation algorithm. Asia Pacific J Atmos Sci 46(2):173–183

    Article  Google Scholar 

  • Chaudhuri S, De Sarkar A (2009) Severity of tropical cyclones atypical during E1 Nino: a statistical elucidation. Asian J Water Environ Pollut 6(4):79–85

    Google Scholar 

  • Chaudhuri S, Middey A (2011) Adaptive neuro-fuzzy inference system to forecast peak gust speed during thunderstorms. Met Atmos Phys 114:139–149

    Article  Google Scholar 

  • Chaudhuri S, Middey A, Goswami S, Banerjee S (2012) Appraisal of the prevalence of severe tropical storms over Indian Ocean by screening the features of tropical depressions. Nat Hazards 61(2):745–756

    Article  Google Scholar 

  • Chaudhuri S, Dutta D, Goswami S, Middey A (2013) Intensity forecast of tropical cyclones over North Indian Ocean using multi layer perceptron model: skill and performance verification. Nat Hazards 65:97–113

    Google Scholar 

  • Dvorak VF (1975) Tropical cyclone intensity analysis and forecasting from satellite imagery. Mon Weather Rev 103(5):420–430

    Article  Google Scholar 

  • Elsberry RL, Lambert TDB, Boothe MA (2007) Accuracy of Atlantic and eastern north Pacific tropical cyclone intensity forecast guidance. Weather Forecast 22:747–762

    Article  Google Scholar 

  • Gardner MW, Dorling SR (1998) Artificial neural networks (the multilayer perceptron)—a review of applications in the atmospheric sciences. Atmos Environ 32:2627–2636

    Article  Google Scholar 

  • Haykin S (1999) Neural networks, a comprehensive foundation, 2nd edn. Prentice Hall, New Jersey

    Google Scholar 

  • Houze RA, Smull BF, Lee WC, Bell MM (2007) Hurricane intensity and eyewall replacement. Science 315:1235–1238

    Article  Google Scholar 

  • Hsieh WW, Tang B (1998) Applying neural network models to prediction and data analysis in meteorology and oceanography. Bull Am Meteor Soc 79:1855–1870

    Article  Google Scholar 

  • India Meteorological Department (2002) Damage Potential of Tropical Cyclones, Published by the office of Additional Director General of Meteorology (Research), IMD Tech Note 71

  • Kidder SQ, Gary WM, Vonder TH (1978) Estimating tropical cyclone central pressure and outer winds from satellite microwave data. Mon Weather Rev 106(10):1458–1464

    Article  Google Scholar 

  • Luo Z, Stephens GL, Emanuel KA, Vane DG, Tourville ND, Haynes JM (2008) On the use of cloud sat and MODIS data for estimating hurricane intensity. IEEE Geo Sci Remote Sens Lett 5(1):13–16

    Article  Google Scholar 

  • Maqsood I, Muhammad RK, Abraham A (2004) Neurocomputing Based Canadian Weather Analysis, Computational Intelligence and Applications. Dynamic Publishers Inc., USA, pp 39–44

    Google Scholar 

  • Pal SK, Mitra S (1999) Neuro-fuzzy pattern recognition: Methods in soft computing. Wiley, New York

    Google Scholar 

  • Perez P, Reyes J (2001) Prediction of particulate air pollution using neural techniques. Neural Comput Appl 10:165–171

    Article  Google Scholar 

  • Rao KN, Jayaraman S (1958) A statistical study of frequency of depressions/cyclone in the Bay of Bengal. Indian J Meteorol Geophys 9:233–250

    Google Scholar 

  • Velden CS (2006) The Dvorak tropical cyclone intensity estimation technique: a satellite-based method that has endured for over 30 years. Bull Am Meteorol Soc 87(9):1195–1210

    Article  Google Scholar 

  • Wedge et al (2005) On neural network architectures and overtopping. Proc Inst Civil Eng Maritime Eng 14015:1–11

    Google Scholar 

  • WMO technical document No. 84 (2010) Tropical cyclone programme, TCP-21, Tropical Cyclone operational plan for the Bay of Bengal and the Arabian Sea

  • Wong V, Emanuel KA (2007) Use of cloud radars and radiometers for tropical cyclone intensity estimation. Geophys Res Lett 34(12). doi:10.1029/2007GL029960

Download references

Acknowledgments

The authors thank IMD, GOI and NOAA for making the data available for research. The authors thank the anonymous reviewers for constructive comments and suggestions.

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Correspondence to Sutapa Chaudhuri.

Appendix: Statistical skill score parameters (Chaudhuri and Middey 2011; Chaudhuri et al. 2012)

Appendix: Statistical skill score parameters (Chaudhuri and Middey 2011; Chaudhuri et al. 2012)

Probability of detection (POD), \( {\text{POD}} = \frac{a}{(a + c)} \)

Critical success index (CSI), \( {\text{CSI}} = \frac{a}{(a + b + c)} \)

Hit rate (HR), \( {\text{HR}} = \frac{(a + d)}{n} \)

False alarm ratio (FAR), \( {\text{FAR}} = \frac{b}{(a + b)} \)

Yule’s Q, \( {\text{Yule's}}\,Q = \frac{(ad - bc)}{(ad + bc)} \)

True skill statistic (TSS), \( {\text{TSS}} = \frac{(ad - bc)}{(a + c)(b + d)} \) Heidke skill score (HSS), \( {\text{HSS}} = \frac{2(ad - bc)}{{\left[ {(a + c)(c + d) + (a + b)(b + d)} \right]}} \) where “a” is the number of times that forecast “Yes” matched with observed “Yes”, “b” is the number of times that forecast “Yes” did not match with observation, “c” is the number of times that forecast is “No” but observation is “Yes,” and “d” is the number of times that forecast “No” matched with the observation “No”(Table 6).

Table 6 Model contingency table for computation of forecast quality

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Chaudhuri, S., Goswami, S. & Middey, A. Medium-range forecast of cyclogenesis over North Indian Ocean with multilayer perceptron model using satellite data. Nat Hazards 70, 173–193 (2014). https://doi.org/10.1007/s11069-013-0805-9

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