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Assimilation of Doppler Weather Radar Data in WRF Model for Simulation of Tropical Cyclone Aila

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Abstract

For the accurate and effective forecasting of a cyclone, it is critical to have accurate initial structure of the cyclone in numerical models. In this study, Kolkata Doppler weather radar (DWR) data were assimilated for the numerical simulation of a land-falling Tropical Cyclone Aila (2009) in the Bay of Bengal. To study the impact of radar data on very short-range forecasting of a cyclone's path, intensity and precipitation, both reflectivity and radial velocity were assimilated into the weather research and forecasting (WRF) model through the ARPS data assimilation system (ADAS) and cloud analysis procedure. Numerical experiment results indicated that radar data assimilation significantly improved the simulated structure of Cyclone Aila. Strong influences on hydrometeor structures of the initial vortex and precipitation pattern were observed when radar reflectivity data was assimilated, but a relatively small impact was observed on the wind fields at all height levels. The assimilation of radar wind data significantly improved the prediction of divergence/convergence conditions over the cyclone's inner-core area, as well as its wind field in the low-to-middle troposphere (600–900 hPa), but relatively less impact was observed on analyzed moisture field. Maximum surface wind speed produced from DWR–Vr and DWR–ZVr data assimilation experiments were very close to real-time values. The impact of radar data, after final analysis, on minimum sea level pressure was relatively less because the ADAS system does not adjust for pressure due to the lack of pressure observations, and from not using a 3DVAR balance condition that includes pressure. The greatest impact of radar data on forecasting was realized when both reflectivity and wind data (DWR–ZVr and DWR–ZVr00 experiment) were assimilated. It is concluded that after final analysis, the center of the cyclone was relocated very close to the observed position, and simulated cyclone maintained its intensity for a longer duration. Using this analysis, different stages of the cyclone are better captured, and cyclone structure, intensification, direction of movement, speed and location are significantly improved when both radar reflectivity and wind data are assimilated. As compared to other experiments, the maximum reduction in track error was noticed in the DWR–ZVr and DWR–ZVr00 experiments, and the predicted track in these experiments was very close to the observed track. In the DWR–ZVr and DWR–ZVr00 experiments, rainfall pattern and amount of rainfall forecasts were remarkably improved and were similar to the observation over West Bengal, Orissa and Jharkhand; however, the rainfall over Meghalaya and Bangladesh was missed in all the experiments. The influence of radar data reduces beyond a 12-h forecast, due to the dominance of the flow from large-scale, global forecast system models. This study also demonstrates successful coupling of the data assimilation package ADAS with the WRF model for Indian DWR data.

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Acknowledgments

The authors are thankful to Guru Gobind Singh Indraprastha University, New Delhi, for support in carrying out this study. The authors are also grateful to the Director General of Meteorology, IMD, New Delhi, for encouragement in carrying out this work. The authors gratefully acknowledge the radar unit at H/Q, DWR Kolkata, NWP Division (IMD, New Delhi), NCEP (USA), NWP system (ARPS) of CAPS, University of Oklahoma (USA), the WRF model of NCAR (USA), and the HPCS system, IMD (New Delhi) for assistance in this study.

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  1. India Meteorological Department, Lodi Road, New Delhi, 110003, India

    Kuldeep Srivastava

  2. Guru Gobind Singh Indraprastha University, Dwarka, New Delhi, India

    Rashmi Bhardwaj

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  1. Kuldeep Srivastava
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  2. Rashmi Bhardwaj
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Correspondence to Rashmi Bhardwaj.

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Srivastava, K., Bhardwaj, R. Assimilation of Doppler Weather Radar Data in WRF Model for Simulation of Tropical Cyclone Aila. Pure Appl. Geophys. 171, 2043–2072 (2014). https://doi.org/10.1007/s00024-013-0723-5

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