Abstract
An extended range tropical cyclogenesis forecast model has been developed using the forecasts of global models available from TIGGE portal. A scheme has been developed to detect the signatures of cyclogenesis in the global model forecast fields [i.e., the mean sea level pressure and surface winds (10 m horizontal winds)]. For this, a wind matching index was determined between the synthetic cyclonic wind fields and the forecast wind fields. The thresholds of 0.4 for wind matching index and 1005 hpa for pressure were determined to detect the cyclonic systems. These detected cyclonic systems in the study region are classified into different cyclone categories based on their intensity (maximum wind speed). The forecasts of up to 15 days from three global models viz., ECMWF, NCEP and UKMO have been used to predict cyclogenesis based on multi-model ensemble approach. The occurrence of cyclonic events of different categories in all the forecast steps in the grided region (10 × 10 km2) was used to estimate the probability of the formation of cyclogenesis. The probability of cyclogenesis was estimated by computing the grid score using the wind matching index by each model and at each forecast step and convolving it with Gaussian filter. The proposed method is used to predict the cyclogenesis of five named tropical cyclones formed during the year 2013 in the north Indian Ocean. The 6–8 days advance cyclogenesis of theses systems were predicted using the above approach. The mean lead prediction time for the cyclogenesis event of the proposed model has been found as 7 days.
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The authors are thankful to the THORPEX Interactive Grand Global Ensemble (TIGGE) (http://tigge-portal.ecmwf.int) for providing the free access to the global model output.
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Jaiswal, N., Kishtawal, C.M., Bhomia, S. et al. Multi-model ensemble-based probabilistic prediction of tropical cyclogenesis using TIGGE model forecasts. Meteorol Atmos Phys 128, 601–611 (2016). https://doi.org/10.1007/s00703-016-0436-2
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DOI: https://doi.org/10.1007/s00703-016-0436-2