what were the causes of fani cyclone?
Answers
Answer:
The IMD began tracking a depression located west of Sumatra on 26 April, classifying it as BOB 02. Later that day, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system.[7] Afterward, the storm slowly coalesced while moving northward, and was upgraded to a deep depression at 00:00 UTC on 27 April.[8] At the same time, the JTWC began warning on the system, designating it 01B.[9] Six hours later, the IMD upgraded the system to a cyclonic storm and gave it the name Fani.[10]
The system continued to intensify until 18:00 UTC on 17 April, after which it stagnated for over a day, as convection around the storm's center waxed and waned.[11] Fani resumed strengthening around 12:00 UTC, with the IMD upgrading it to a severe cyclonic storm.[12] At that time, Fani began a period of rapid intensification as it was located within a very favorable environment with sea surface temperatures of 30–31 °C (86–88 °F) and low vertical wind shear. As a result, the JTWC upgraded Fani to a Category 1-equivalent cyclone late on 29 April.[13] Around 00:00 UTC on 30 April, Fani was upgraded to a very severe cyclonic storm by the IMD.[14] The organization of the system continued to improve, with tight spiral banding wrapping into a formative eye feature,[15] resulting in Fani being upgraded to an extremely severe cyclonic storm by the IMD around 12:00 UTC[16] while the JTWC upgraded the storm to a Category 3-equivalent cyclone hours later.[17] Development proceeded more slowly over the following days, with little improvement evident in the system's satellite presentation. On 2 May, however, the central dense overcast became more symmetrical and the eye more distinct, and Fani was upgraded to a Category 4-equivalent cyclone by the JTWC at 06:00 UTC.[18] Shortly after, Fani started another period of rapid intensification, attaining 1-minute sustained winds of 250 km/h (155 mph) just below Category 5-equivalent tropical cyclone intensity, according to the JTWC.[19] At 8:00 a.m. IST (02:30 UTC) 3 May, Fani made landfall near Puri, Odisha as a severe cyclonic storm, with 3-minute sustained winds of 185 km/h (115 mph).[20] This made Fani the most intense storm to make landfall in India's Odisha state since the 1999 Odisha cyclone.[21] Land interaction quickly degraded Fani's convective structure; and it weakened to a Category 1-equivalent tropical cyclone soon after landfall.[22] Fani continued to weaken after landfall, weakening to a cyclonic storm later that day,[23] before passing just north of Kolkata. On 4 May, Fani weakened to a deep depression and moved into Bangladesh,[24] before degenerating into a well-marked low later on the same day.[25] On 5 May, Fani's remnant low dissipated over Bhutan
Answer:
It cause many problems to the odissa peoples it came many people die