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Pakistan flood : ウィキペディア英語版
2010 Pakistan floods

The floods in Pakistan began in late July 2010, resulting from heavy monsoon rains in the Khyber Pakhtunkhwa, Sindh, Punjab and, Balochistan regions of Pakistan, which affected the Indus River basin. Approximately one-fifth of Pakistan's total land area was underwater, approximately . According to Pakistani government data, the floods directly affected about 20 million people, mostly by destruction of property, livelihood and infrastructure, with a death toll of close to 2,000.〔
UN Secretary-General Ban Ki-moon had initially asked for US$460 million (€420 million) for emergency relief, noting that the flood was the worst disaster he had ever seen. Only 20% of the relief funds requested had been received on 15 August 2010. The U.N. had been concerned that aid was not arriving fast enough, and the World Health Organization reported that ten million people were forced to drink unsafe water. The Pakistani economy was harmed by extensive damage to infrastructure and crops. Damage to structures was estimated to exceed US$4 billion (€2.5 billion), and wheat crop damages were estimated to be over US$500 million (€425 million). Total economic impact may have been as much as US$43 billion (€35 billion).〔 〕
==Causes==
The floods were driven by rain. The rainfall anomaly map published by NASA showed unusually intense monsoon rains attributed to La Niña. On 21 June, the Pakistan Meteorological Department cautioned that urban and flash flooding could occur from July to September in the north parts of the country.〔(【引用サイトリンク】url=http://pakmet.com.pk/MON&TC/Monsoon/monsoon(2010).html )〕 The same department recorded above-average rainfall in the months of July and August 2010 and monitored the flood wave progression. Discharge levels were comparable to those of the floods of 1988, 1995, and 1997. The monsoon rainfall of 2010 over the whole country was the highest since 1994 and the second highest during last 50 years.
A research by Utah State University〔Wang et al. (2011) http://onlinelibrary.wiley.com/doi/10.1029/2011JD015760/abstract〕 analyzed conditional instability, moisture flux, and circulation features and the results support a persistent increase in conditional instability during the July premonsoon phase, accompanied by increased frequency of heavy rainfall events. The increased convective activity during the premonsoon phase agrees with the projected increase in the intensity of heavy rainfall events over northern Pakistan. Large-scale circulation analysis reveals an upper-level cyclonic anomaly over and to the west of Pakistan〔(【引用サイトリンク】title=Identification of extreme precipitation threat across midlatitude regions based on short-wave circulations )〕–a feature empirically associated with weak monsoon. The analysis also suggests that the anomalous circulation in 2010 is not sporadic but rather is part of a long-term trend that defies the typical linkage of strong monsoons with an anomalous anticyclone in the upper troposphere.
An article in the ''New Scientist'' attributed the cause of the exceptional rainfall to "freezing" of the jet stream, a phenomenon that reportedly also caused unprecedented heat waves and wildfires in Russia as well as the 2007 United Kingdom floods.
In response to previous Indus River floods in 1973 and 1976, Pakistan created the Federal Flood Commission (FFC) in 1977. The FFC operates under Pakistan's Ministry of Water and Power. It is charged with executing flood control projects and protecting lives and property of Pakistanis from the impact of floods. Since its inception the FFC has received Rs 87.8 billion (about 900 million USD). FFC documents show that numerous projects were initiated, funded and completed, but reports indicate that little work has actually been done due to ineffective leadership and corruption.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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