Question: What is the name of the Cyclone that delayed the work of Minjur Seawater Desalination Plant and was the ninth tropical cyclone of the 2008 North Indian Ocean cyclone season?
Context: The Minjur Desalination Plant is a reverse osmosis, water desalination plant at Kattupalli village, a northern suburb of Chennai, India, on the coast of the Bay of Bengal that supplies water to the city of Chennai.  Built on a 60-acre site, it is the largest desalination plant in India.  Construction works were carried out by Indian company IVRCL and the Spanish Abengoa under the direction of the Project Manager Fernando Portillo Vallés and the Construction Manager Juan Ignacio Jiménez-Velasco, who returned to Europe after the inauguration of the plant to work on Renewable Energy Projects.  Originally scheduled to be operational by January 2009, the work on the plant was delayed due to Cyclone Nisha in October 2008, which damaged a portion of the completed marine works and destroyed the cofferdam meant for the installation of transition pipes.  The trial runs were completed in June 2010 and the plant was opened in July 2010.  Water from the plant will be utilised chiefly for industrial purposes such as the Ennore Port and North Chennai Thermal Power Station.  However, during droughts, water from the plant will be supplied to public, serving an estimated population of 1,000,000. The 2011 North Indian Ocean cyclone season was the "least active" tropical cyclone season in the North Indian Ocean since 1993.  Only two cyclone storms have formed throughout the year, far below the average of 4-6.  The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November.  These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.  The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula.  There are two main seas in the North Indian Ocean — the Arabian Sea to the west of the Indian subcontinent, abbreviated "ARB" by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated "BOB" by the IMD. The 1999 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation.  The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November.  These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. Cyclone Nisha (IMD designation: BOB 07, JTWC designation: 06B, also known as Cyclonic Storm Nisha) was the ninth tropical cyclone of the 2008 North Indian Ocean cyclone season, and the seventh tropical cyclone in the Bay of Bengal that year.  A fairly weak tropical cyclone, it caused some notable damage in India and Sri Lanka. The 2010 North Indian Ocean cyclone season was the "most intense" tropical cyclone season in the North Indian Ocean since the 1998 North Indian Ocean cyclone season.  The season saw 8 depressions and 5 named storms forming in the region. The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation.  The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November.  These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The 2016 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation.  It was the deadliest season since 2010, killing about 400 people.  The season was an average one, seeing four named storms, with one further intensifying into a very severe cyclonic storm.  The first named storm, Roanu, developed on May 19 while the season's last named storm, Vardah, dissipated on December 13.  The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November.  These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. In October 2008, the remnants of a tropical cyclone caused extensive damage in Yemen, a poor country on the southern tip of the Arabian Peninsula.  The storm, officially known as Deep Depression ARB 02, was the sixth tropical cyclone of the 2008 North Indian Ocean cyclone season, and the second tropical cyclone in the Arabian Sea that year.  It formed on October 19 off the west coast of India from the same broader system that spawned a storm in the southern Indian Ocean.  Moving generally westward, the depression failed to intensify much, reaching maximum sustained winds of only 55 km/h (35 mph).  It was no longer classifiable as a tropical depression by October 23, and later that day, its remnants struck near Ash Shihr in eastern Yemen. Tropical Cyclone Kesiny was the first recorded tropical cyclone – the equivalent of a minimal hurricane – to make landfall in the month of May 2002 in the south-west Indian Ocean.  The final named storm of the busy 2001–02 South-West Indian Ocean cyclone season, Kesiny formed on May 2 from a trough near the equator.  Its formation was the result of an increase in the Madden–Julian oscillation, which also contributed to a twin storm in the north Indian Ocean that hit Oman, and another set of storms in northeast and southeast Indian Ocean.  Kesiny initially moved to the southeast, but later turned to the southwest due to a strengthening ridge.  On May 6, it intensified into a tropical cyclone, but later weakened and was not expected to re-strengthen.  However, Kesiny developed an eye and re-intensified into a tropical cyclone on May 9, reaching peak winds of 130 km/h before striking Madagascar about 60 km southeast of Antsiranana.  It weakened while crossing the country, and after turning to the south it struck the country again before dissipating on May 11. The 2007 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation.  The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November.  These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Answer: Cyclone Nisha