Question: Considered the strongest recorded tropical cyclone, which cyclone had a film made about it in 2007?

<P0-S0> Super Cyclonic Storm Gonu (also simply known as Cyclone Gonu) is the strongest tropical cyclone on record in the Arabian Sea, and is also the strongest named cyclone in the northern Indian Ocean. <P0-S1>  The second named tropical cyclone of the 2007 North Indian Ocean cyclone season, Gonu developed from a persistent area of convection in the eastern Arabian Sea on June 1, 2007. <P0-S2>  With a favorable upper-level environment and warm sea surface temperatures, it rapidly intensified to attain peak winds of 235 km/h (145 mph) on June 4, according to the India Meteorological Department. <P0-S3>  Gonu weakened after encountering dry air and cooler waters, and early on June 6, it made landfall on the easternmost tip of Oman, becoming the strongest tropical cyclone to hit the Arabian Peninsula. <P0-S4>  It then turned northward into the Gulf of Oman, and dissipated on June 7 after making landfall in southern Iran, the first landfall in the country since 1898. <SEP> <P1-S0> Kathantara (Odia: କଥାନ୍ତର , English "Another Story") is a 2007 Indian Oriya language disaster film directed by Himansu Khatua, a story of tribulations of the 1999 Odisha cyclone. <SEP> <P2-S0> Severe Tropical Cyclone Esau became the strongest tropical cyclone to affect New Caledonia on record during February and March 1992. <P2-S1>  A shallow tropical depression developed within the monsoon trough during 24 February, about 370  km (230 mi) to the northeast of Port Vila, Vanuatu. <P2-S2>  Over the next day the system gradually developed further as it moved towards the south-west under the influence of a northerly steering flow, before it passed over Pentecost Island in northern Vanuatu during 25 February. <P2-S3>  After passing over Pentecost the system continued to move towards the southwest and passed near the island of Malampa, before the depression turned northwards and executed a small clockwise loop as it passed over the island of Espiritu Santo. <P2-S4>  The system was subsequently named Esau during 26 February, after it had developed into a tropical cyclone. <P2-S5>  Over the next couple of days the system moved south-westwards towards Australia and away from the islands of Vanuatu. <P2-S6>  Esau subsequently executed a second clockwise loop during 28 February, before it peaked as a Category 4 tropical cyclone on both the Australian tropical cyclone intensity scale and the Saffir-Simpson hurricane wind scale. <P2-S7>  After it had peaked the system moved south-eastwards and threatened Southern Vanuatu, before turning southwards and threatening the French overseas territory of New Caledonia. <P2-S8>  Esau made landfall on the French territory during 4 March, as a category 3 severe tropical cyclone before degenerating into an extratropical cyclone during 5 March. <P2-S9>  The systems remnants made landfall on New Zealand's North Island during 8 March, before they were last noted during the next day over the South Pacific Ocean. <SEP> <P3-S0> The 1999 Odisha cyclone (IMD designation BOB 03, JTWC designation 05B) was the strongest recorded tropical cyclone in the North Indian Ocean and among the most destructive in the region. <P3-S1>  The 1999 Odisha cyclone organized into a tropical depression in the Andaman Sea on 25 October, though its origins could be traced back to an area of storms in the Sulu Sea four days prior. <P3-S2>  The disturbance gradually strengthened as it took a west-northwesterly path, reaching cyclonic storm strength the next day. <P3-S3>  Taking advantage of highly favorable conditions, the storm rapidly intensified, attaining super cyclonic storm intensity on 28 October before peaking with winds of 260 km/h (160 mph) and a record-low pressure of 912 mbar (hPa; 26.93 inHg). <P3-S4>  The storm maintained this intensity as it made landfall on Odisha on 29 October. <P3-S5>  The cyclone steadily weakened due to persistent land interaction and dry air, remaining quasi-stationary for two days before slowly drifting offshore as a much weaker system; the storm dissipated on 1 November over the Bay of Bengal.