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The 2006 North Indian Ocean cyclone season had no 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 basin is north of the Equator and west of the Malay Peninsula. The IMD and JTWC monitor this basin. This basin is divided in two seas by India, the Bay of Bengal and Arabian Sea, abrriviated ''BOB'' and ''ARB'', respectively. Although an inactive year, 2006 had more of note than previous years like 2005 or 2004. Cyclone Mala caused severe damage and killed 22 when it hit Burma as a cat. 3. An unnamed depression killed over 100 in India, and cyclonic storm Ogni caused minor effects in India as well. Additionally, the remnants of Typhoon Durian crossed the Malay Peninsula causing minor effects, but was a rare basin-crosser in this area. == Season summary == ImageSize = width:850 height:200 PlotArea = top:10 bottom:80 right:50 left:20 Legend = columns:3 left:30 top:58 columnwidth:270 AlignBars = early DateFormat = dd/mm/yyyy Period = from:01/01/2013 till:01/01/2014 TimeAxis = orientation:horizontal ScaleMinor = grid:black unit:month increment:1 start:01/01/2013 Colors = id:canvas value:gray(0.88) id:GP value:red id:TD value:rgb(0.5,0.8,1) legend:Depression id:DD value:rgb(0.37,0.73,1) legend:Deep_Depression id:TS value:rgb(0,0.98,0.96) legend:Cyclonic_Storm id:ST value:rgb(0.8,1,1) legend:Severe_Cyclonic_Storm id:VS value:rgb(1,0.76,0.25) legend:Very_Severe_Cyclonic_Storm id:ES value:rgb(1,0.56,0.13) legend:Extremely_Severe_Cyclonic_Storm id:SU value:rgb(1,0.38,0.38) legend:Super_Cyclonic_Storm Backgroundcolors = canvas:canvas BarData = barset:Hurricane bar:Month PlotData= barset:Hurricane width:10 align:left fontsize:S shift:(4,-4) anchor:till from:13/01/2013 till:14/01/2013 color:DD text:"ARB 01" from:25/04/2013 till:29/04/2013 color:ES text:"Mala" from:02/07/2013 till:05/07/2013 color:DD text:"BOB 02" from:02/08/2013 till:05/08/2013 color:DD text:"BOB 03" from:12/08/2013 till:13/08/2013 color:TD text:"BOB 04" barset:break from:16/08/2013 till:18/08/2013 color:TD text:"BOB 05" from:29/08/2013 till:01/09/2013 color:TD text:"BOB 06" from:03/09/2013 till:04/09/2013 color:TD text:"BOB 07" from:21/09/2013 till:24/09/2013 color:TD text:"Land 01" from:21/09/2013 till:24/09/2013 color:ST text:"Mukda" barset:break from:28/09/2013 till:30/09/2013 color:TD text:"BOB 08" from:29/10/2013 till:30/10/2013 color:TS text:"Ogni" from:05/12/2013 till:06/12/2013 color:TD text:"Durian" bar:Month width:5 align:center fontsize:S shift:(0,-20) anchor:middle color:canvas from:01/01/2013 till:31/01/2013 text:January from:01/02/2013 till:28/02/2013 text:February from:01/03/2013 till:31/03/2013 text:March from:01/04/2013 till:30/04/2013 text:April from:01/05/2013 till:31/05/2013 text:May from:01/06/2013 till:30/06/2013 text:June from:01/07/2013 till:31/07/2013 text:July from:01/08/2013 till:31/08/2013 text:August from:01/09/2013 till:30/09/2013 text:September from:01/10/2013 till:31/10/2013 text:October from:01/11/2013 till:30/11/2013 text:November from:01/12/2013 till:31/12/2013 text:December Overall activity across the North Indian Ocean during 2006 was slightly below-average, with 12 depressions, 3 cyclonic storms, and 1 very severe cyclonic storm. An average season, according to the IMD, consists of 15 depressions and 5–6 cyclonic storms. In addition to the storms monitored by the IMD, the JTWC also tracked the remnants of Typhoon Durian across the Malay Peninsula into the Andaman Sea as a tropical depression in early December. The majority of storms formed within the Bay of Bengal, with only two existing in the Arabian Sea. Activity peaked during the summer due to an active southwest monsoon.〔〔 Starting in May, the seasonal monsoon developed over the Bay of Bengal and advanced northwestward over India where it propagated through September. During this period the system spawned numerous disturbances, nine of which became tropical cyclones. All but one of these systems formed in the northern Bay of Bengal and struck Odisha before spreading rain across large portions of India. The outlier was Severe Cyclonic Storm Mukda in late September which remained virtually stationary its entire existence to the southwest of Gujarat. The combined effects of the eight other depressions along with the monsoon itself caused disastrous flooding throughout India. By early August, nearly 500,000 people were evacuated in Mumbai due to rising waters. The collective effects of the depressions alone resulted in at least 562 fatalities with hundreds more attributed to the monsoon rains.〔 More than 1 million people across Odisha were left homeless from the storms. During periods of cyclonic activity, rainfall associated with the monsoon was above-average as a whole. Departures from average reached 13.8%, 26.2%, 28.1%, 9.8%, and 11.5% for the periods of July 5–12 (BOB 02), August 2–9 (BOB 03), August 9–16 (BOB 04), September 20–27 (Land 01 and Mukda), and September 27–October 5 (BOB 08), respectively.〔〔 In contrast to the notable activity of the monsoon in respect to tropical cyclone formation, rainfall from the monsoon across India was predominantly below-average due to poor distribution of rain. Of the four broadly defined regions of India used by the IMD, only Central India experienced above-average rainfall, possibly due to the multiple cyclones that passed through the region. This area received an average of of rain between June and September, while the average is . In addition, five sub-divisions (the Andaman and Nicobar Islands, Arunachal Pradesh, Assam and Meghalaya, west Uttar Pradesh, and Haryana) experienced drought conditions.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「2006 North Indian Ocean cyclone season」の詳細全文を読む スポンサード リンク
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