Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS04] Machine Learning Techniques in Weather, Climate, Hydrology and Disease Predictions

Fri. Jun 4, 2021 3:30 PM - 5:00 PM Ch.10 (Zoom Room 10)

convener:Venkata Ratnam Jayanthi(Application Laboratory, JAMSTEC), Rajib Maity(Indian Institute of Technology Kharagpur), Swadhin Behera(Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001), Takeshi Doi(JAMSTEC), Chairperson:Pascal Oettli(Japan Agency for Marine-Earth Science and Technology), Venkata Ratnam Jayanthi(Application Laboratory, JAMSTEC), Takeshi Doi(JAMSTEC), Swadhin Behera(Application Laboratory, JAMSTEC, 3173-25 Showa-machi, Yokohama 236-0001)

4:15 PM - 4:30 PM

[AAS04-10] Forecasting Standardized Precipitation Evapotranspiration Index (SPEI) Using Multilayer Perceptron Artificial Neural Network Model for Central India

*Sourabh Shrivastava1,2, R. Uday Kiran1, P K Bal3, K K Singh4, Tomohito Yamada2 (1.University of Aizu, 2.Hokkaido University , 3.Qatar Meteorology Department, 4.India Meteorological Department)

Keywords:Artificial Neural Network, SPEI, Drought, ROC Curve

This study presents an Artificial Neural Network approach to estimate the drought events in an Indian state of Madhya Pradesh. Sea Surface Temperatures data obtained from Centennial Observation-Based Estimates (COBE) and seasonal rainfall data (June-August) obtained from India Meteorological Department for the period 1971 to 2013 are used in this study to develop two different ANN models, aiming to forecast the standardized precipitation evapotranspiration index at four different stations in Madhya Pradesh. Preliminary results from the first ANN model (derived from SST only) showed that correlation between observed SPEI and SST ranged between 0.585 to 0.773 where as in case of the second ANN model (derived from both rainfall and SST), the correlation remains between 0.960 to 0.979. Further, coefficient of determination remains in the range 0.312 to 0.591 and 0.919 to 0.958 for the 1st ANN and second ANN model respectively. Furthermore, probabilistic forecasts of SPEI are made and the relative operating characteristics scores are examined and the results indicate that the forecast results from the SPEI values are suitable for various meteorological application and ANNs offer a framework for forecasting the SPEI drought index in the absence of observed rainfall data.