Research Article
Role of Four-Dimensional Data Assimilation on Track and Intensity of Severe Cyclonic Storms
Table 1
Comparison of observed parameters with simulated parameters for cyclone Aila and Jal.
| Cyclone | Experiment | Landfall time | Landfall Position | CSLP (hPa) | MSW (m/s) |
| Aila | Observed (IMD) | 08 and 09 UTC of May 25 | 88E/21.8N | 968 | 30.84 | WRF with FDDA | 06 UTC of May 25 2009 | 88E/21.73N | 976 | 34 | Without FDDA | Bet. 9–12 UTC of May 25 | 87.13E/20.37N | 962 | 36 |
| Jal | Observed (IMD) | Near 16 UTC of Nov. 7 | 80.2E/13.3N | 988 | 30.84 | WRF with FDDA | Near 06 UTC of Nov. 7 | 80.16E/13.67N | 976 | 40 | Without FDDA | Bet. 6–12 UTC of Nov. 7 | 79.54E/14.6N | 978 | 40 |
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