 The cyclone shortly before peak intensity on May 23 | |
| Meteorological history | |
|---|---|
| Formed | May 21, 2001 |
| Dissipated | May 29, 2001 |
| Extremely severe cyclonic storm | |
| 3-minute sustained (IMD) | |
| Highest winds | 215 km/h (130 mph) |
| Lowest pressure | 932 hPa (mbar); 27.52 inHg |
| Category 3-equivalent tropical cyclone | |
| 1-minute sustained (SSHWS/JTWC) | |
| Highest winds | 205 km/h (125 mph) |
| Lowest pressure | 927 hPa (mbar); 27.37 inHg |
| Overall effects | |
| Casualties | 120–900 dead or missing |
| Damage | Minimal |
| Areas affected | Western India |
| IBTrACS / [1] | |
Part of the 2001 North Indian Ocean cyclone season | |
The 2001 Gujarat cyclone was the third strongest tropical cyclone, in terms of barometric pressure, to form in the Arabian Sea on record; only Cyclones Gonu in 2007 and Kyarr in 2019 were stronger. The storm originated from a tropical disturbance that formed east of Somalia on May 18. Over the following few days, the system gradually organized into a tropical depression. Tracking eastward, towards the coastline of southwestern India, the storm slowly intensified. Shortly before reaching shore, the system turned north and later west, away from land. After taking this turn, the storm intensified into a very severe cyclonic storm, attaining its peak intensity on May 24 with winds of 215 km/h (130 mph 3-minute winds) and a barometric pressure of 932 mbar (hPa). At the time, this ranked the cyclone as the strongest known storm in the Arabian Sea.
After stalling several hundred kilometres offshore, the storm weakened over cooler waters that it had upwelled. By May 27, the system weakened to a cyclonic storm and by this time was approaching the northwestern coastline of India, near Gujarat. The following day, the storm made landfall in the Saurashtra region as a deep depression with winds of 55 km/h (35 mph 3-minute winds). The depression quickly weakened after moving inland and dissipated early on May 29.
Although a powerful cyclone over water, the storm had relatively little impact over land. In the Valsad district, two coastal communities lost a combined 200 homes due to large swells produced by the storm. However, the losses were more extensive offshore. Between 120 and 900 fishermen were listed as missing after contact was lost with their vessels during the storm.