On June 7, small area of low pressure developed off the west coast of India. Over the following two days, convection associated with the low gradually organized and by June 9, satellite intensity estimates from the JTWC reached 55 km/h (30 mph). A TCFA was subsequently issued for the system before it made landfall in Gujarat early on June 10. Although overland, the low maintained significant convection as it turned westward and through its re-emergence into the Arabian Sea on June 11. Once back over water, convection rapidly spread westward in response to an anticyclone over the Arabian Peninsula and Afghanistan. Early on June 12, the cyclone was estimated to have attained tropical storm status based on a ship report near the center of 65 km/h (40 mph) sustained winds and a surface pressure of 998 mbar (hPa; 29.47 inHg). Later that day, strong wind shear stemming from the anticyclone displaced convection from the tropical storm by more than 110 km (70 mi), prompting the final advisory from the JTWC. The remnants of the system were last noted on June 13, dissipating over the Arabian Sea.