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Cyclone Phet

North Indian cyclone in 2010

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Through Western India, Monsoon and High-pressure area

After exiting Oman on 4 June, Phet turned to the northeast and later to the east while continuing to weaken. The residual thunderstorms spread ahead of the circulation over Pakistan, producing 370 mm (15 in) of rainfall at Gwadar. In the city, the storm washed away houses and flooded the port, On June 6, Phet moved ashore the country near Karachi, a city of 16 million people, where several neighborhoods were flooded and power outages lasted over 12 hours. Across Pakistan, the storm killed 16 people and left $81 million in damage. Phet continued into western India, where it degenerated into a remnant low-pressure area. In the country, storm rainfall killed five people, as well as dozens of animals.

Meteorological history

Toward the end of May 2010, a surge in the monsoon produced widespread convection, or thunderstorms, off the southwest coast of India in the southeastern Arabian Sea. After a low-level circulation became evident on 30 May, the India Meteorological Department (IMD) designated the system as a low-pressure area. The low moved northwestward within an area of warm water temperatures of 30 to 32 °C (86 to 90 °F), moderate wind shear, and an upper-level environment conducive for tropical cyclogenesis, The Joint Typhoon Warning Center (JTWC) first noted the system on 30 May as an area of potential development. The circulation became more defined within the building convection, which was amplified by outflow from an anticyclone over the northern Arabian Sea. At 03:00 Coordinated Universal Time (UTC) on 31 May, the IMD designated the system as a depression about 1,000 km (620 mi) west-southwest of Mumbai, India, or about 1,260 km (785 mi) southeast of Muscat, Oman. At 18:00 UTC, the JTWC began issuing advisories on the storm, designating it as Tropical Cyclone 03A.

As the wind shear decreased, the convection increased further, and the IMD upgraded the system to a deep depression at 00:00 UTC on 1 June. Later that day, the system began rapidly intensifying while moving on a northwest trajectory; the IMD upgraded the system to a cyclonic storm at 09:00 UTC, naming it Phet. An eye became evident during a Tropical Rainfall Measuring Mission (TRMM) pass of the storm; its appearance and the development of rainbands showed Phet was intensifying. Late on 1 June, the JTWC upgraded the storm to the equivalent of a minimal hurricane, estimating 1 minute maximum sustained winds of 120 km/h (75 mph), after the eye became better defined and the tightly curved thunderstorm activity. The IMD upgraded Phet to severe cyclonic storm status at 00:00 UTC on 2 June, and further to a very severe cyclonic storm six hours later.

With a ridge to the northeast, the cyclone continued slowly northwestward. The JTWC initially expected that Phet would recurve to the northeast without affecting land, reflecting storm model simulations. Lack of observations across the Arabian Sea prevented more the model forecasts from accurately assessing the ridge. Phet quickly intensified on 2 June as it developed a well-defined 55 km (35 mi) eye, fueled by outflow that was enhanced by a passing mid-latitude trough. At 12:00 UTC on June 2, the IMD estimated peak 3 minute sustained winds of 155 km/h (95 mph). Simultaneously, the JTWC assessed peak 1 minute winds of 230 km/h (145 mph). The agency predicted that Phet would intensify further to reach winds of 260 km/h (160 mph) near the eastern Oman coastline. Drier air from the Arabian Peninsula to the northwest disrupted the storm structure, which caused the eye to become cloud-covered, signaling weakening. Between 00:00–02:00 UTC on 3 June, Phet made landfall in eastern Oman near Al Ashkharah, with winds between 110–120 km/h (70–75 mph) according to the IMD. The JTWC assessed landfall as occurring 16 hours later and with winds of 195 km/h (120 mph).

The cyclone became elongated due to increased wind shear while it turned northeastward around the ridge. High mountains in eastern Oman weakened Phet, causing the structure to become more asymmetrical. At 12:00 UTC on 4 June, the cyclone re-emerged into the Arabian Sea, still presenting banding features and an eye feature but with much less convection. Later that day, the JTWC downgraded Phet to tropical storm status, and by early on 5 June, increased wind shear had displaced the center from the convection. Phet turned eastward once over the Gulf of Oman, weakening to a deep depression by late on 5 June. The circulation remained exposed, producing convection well ahead of the center. At 03:00 UTC on 6 June, the IMD downgraded Phet further to depression status, assessing that the system made landfall at that intensity 12 hours later in southern Pakistan near Karachi. The JTWC discontinued advisories once the storm moved ashore. Phet continued generally eastward, crossing the Pakistan/India in Rajasthan. On 7 June, the depression weakened into a remnant low near Madhya Pradesh.

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