On June 11, 2014, a broad, poorly-defined area of low pressure formed over the South China Sea.
Extensive, though disorganized, deep convection accompanied the system.
Situated within a region of low to moderate wind shear and weak outflow, slow development ensued.
By June 13, the Japan Meteorological Agency (JMA) classified the disturbance as a tropical depression.
A monsoonal system, the depression featured an extensive circulation with the strongest winds well away from the center, contrary to most tropical cyclones.
A scatterometer pass revealed winds up to 65 km/h (40 mph) within a banding feature to the east of the storm's center by the evening of June 13.
In accordance with this, the JMA upgraded the depression to Tropical Storm 1407 and assigned the name Hagibis to the cyclone.
Despite the presence of gale-force winds, the Joint Typhoon Warning Center (JTWC) deemed the system to be below storm intensity and only issued a Tropical Cyclone Formation Alert early on June 14, indicating that it was likely to become a tropical cyclone within 24 hours.
Thereafter, the tropical storm-force winds contracted to within 130 km (80 mi) of the center, indicative of a more tropical than monsoonal system.
As such, the JTWC initiated advisories on the system as Tropical Storm 07W.
Early on June 15, Hagibis made landfall over southern China, and it subsequently weakened to a tropical depression.
On the morning of June 16, both agencies issued their final warnings on Hagibis as it weakened further to a land depression.
Its remnants still continued to move northward, but by June 17, the remnants of Hagibis curved eastwards due to the jet stream.
Later that day, the remnants entered moved back over warm waters, and accompanied by low vertical wind shear, and the storm re-intensified.
The JMA upgraded Hagibis to a tropical storm once again, and both the JTWC and the JMA re-initiated advisories on the system.
Early on June 18, Hagibis transitioned into an extratropical cyclone, and its circulation was absorbed by a developing extratropical storm to the north on June 21.
The system moved out of the basin early on June 23.
On June 11, 2014, a broad, poorly-defined area of low pressure formed over the South China Sea. Extensive, though disorganized, deep convection accompanied the system. Situated within a region of low to moderate wind shear and weak outflow, slow development ensued. By June 13, the Japan Meteorological Agency (JMA) classified the disturbance as a tropical depression. A monsoonal system, the depression featured an extensive circulation with the strongest winds well away from the center, contrary to most tropical cyclones. A scatterometer pass revealed winds up to 65 km/h (40 mph) within a banding feature to the east of the storm's center by the evening of June 13. In accordance with this, the JMA upgraded the depression to Tropical Storm 1407 and assigned the name Hagibis to the cyclone. Despite the presence of gale-force winds, the Joint Typhoon Warning Center (JTWC) deemed the system to be below storm intensity and only issued a Tropical Cyclone Formation Alert early on June 14, indicating that it was likely to become a tropical cyclone within 24 hours. Thereafter, the tropical storm-force winds contracted to within 130 km (80 mi) of the center, indicative of a more tropical than monsoonal system. As such, the JTWC initiated advisories on the system as Tropical Storm 07W.
Early on June 15, Hagibis made landfall over southern China, and it subsequently weakened to a tropical depression. On the morning of June 16, both agencies issued their final warnings on Hagibis as it weakened further to a land depression. Its remnants still continued to move northward, but by June 17, the remnants of Hagibis curved eastwards due to the jet stream. Later that day, the remnants entered moved back over warm waters, and accompanied by low vertical wind shear, and the storm re-intensified. The JMA upgraded Hagibis to a tropical storm once again, and both the JTWC and the JMA re-initiated advisories on the system. Early on June 18, Hagibis transitioned into an extratropical cyclone, and its circulation was absorbed by a developing extratropical storm to the north on June 21. The system moved out of the basin early on June 23.
Tropical Storm Hagibis (2014)