Maharashtra floods of 2005
| Date | 26–27 July 2005 |
|---|---|
| Location | Maharashtra inclusive of Mumbai |
| Deaths | 1094 |
The 2005 Maharashtra floods refers to the flooding of many parts of the Indian state of Maharashtra including large areas of the metropolis Mumbai a city located on the coast of the Arabian Sea, on the Western coast of India, in which approximately 1,094 people died. It occurred just one month after the June 2005 Gujarat floods. The term 26 July, is now always used to refer to the day when the city of Mumbai came to a standstill due to flooding.
A large number of people were stranded on the roads, lost their homes while many walked long distances back home from work that evening. The floods were caused by the eighth heaviest-ever recorded 24-hour rainfall figure of 944 mm (37.17 inches) which lashed the metropolis on 26 July 2005, and intermittently continued for the next day. 644mm (25.35 inches) was received within the 12-hour period between 8am and 8pm. Torrential rainfall continued for the next week. The highest 24-hour period in India was 1,168 mm (46.0 inches) in Aminidivi in the Union Territory of Lakshadweep on 6 May 2004 although some reports suggest that it was a new Indian record. The previous record high rainfall in a 24-hour period for Mumbai was 575 mm (22.6 inches) in 1974.
Other places severely affected were Raigad, Chiplun, [[Khed, Ratna 31 July after heavy rains disrupted the city once again, grounding all flights for the day. Fukuh
On 26 July 2005, around 2:00 p.m. the Mumbai Metropolitan Region was struck by a severe storm and subsequent deluge. The Indian Meteorological Department (IMD) station in Santacruz recorded 944 mm. of rain for the 24 hours ending 8:30 a.m. on 27 July. The Municipal Corporation of Greater Mumbai [MCGM] control room started receiving phone calls reporting the heavy rain and subsequent water logging in suburban areas.
Local train movement came to a halt by 2:30 pm. due to the water-logging on the tracks. This caused traffic on roads to increase dramatically with water logging and submerging of certain low-lying pockets of the region, such as Dharavi, Bandra-Kurla Complex
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