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On August 14, 2016, the National Disaster Risk Reduction and Management Council reported that about 70,000 people, or 15,665 families, were affected by the enhanced monsoon rains in the regions of Central Luzon (Region 3), Calabarzon (Region 4-A), Mimaropa (Region 4-B), Western Visayas (Region 6), the Negros Island Region, the Autonomous Region in Muslim Mindanao, and the National Capital ...
According to Pakistan's NMDA, there were a total of 424 deaths as a result of the pre-monsoon rains (March–May 2016) and monsoon season (June–September 2016). 153 of the people who died were children. By province, Khyber-Pakhtunkhwa was the worst affected during both disasters, with a total of 226 deaths. [29]
2016 Indian floods by monsoon rain India: 2016 1,000 [citation needed] 1961 Bihar flood India: 1961 992 1957 Isahaya flood, massive rain and mudslide Japan: 1957 941 Inuyama Iruka pond dam failure Japan: 1868 933 1938 Hanshin flood, mainly Tokyo, Kobe, massive rain and landslide Japan: 1938 915 Barcelona, flash flood: Spain: 1962 903
The 2016-17 Southern Thailand floods was a large scale flood disaster that occurred in southern Thailand from December 2016 to January 2017. It occurred during the country's annual monsoon season and was characterized as having the "worst rainfall in 30 years". [ 1 ]
Monsoon storms typically form when an area of high pressure draws moisture up from the Baja Peninsula and other parts of Mexico and then the wind turns to blow from the south, pushing that ...
Floods in Thailand are regular natural disasters in Thailand which happen nearly every year during the monsoon season. The monsoon seasons in the country are distinct by region, the southern part mirrors the Malay Peninsula and monsoon begins in October and ends in March. The rest of the nation has monsoons and/or frequent thundershowers from ...
The Voice is officially live!. The Top 8 contestants took the stage for the first live episode of Season 26, in which each hopeful sang twice: a solo performance and a special duet covering a ...
A positive IOD index often negates the effect of ENSO, resulting in increased monsoon rains in years such as 1983, 1994, and 1997. [29] Further, the two poles of the IOD – the eastern pole (around Indonesia) and the western pole (off the African coast) — independently and cumulatively affect the quantity of monsoon rains. [29]
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