Typhoon Ma-on (2011)
http://dbpedia.org/resource/Typhoon_Ma-on_(2011) an entity of type: WikicatTyphoons
平成23年台風第6号（へいせい23ねんたいふうだい6ごう、アジア名：マーゴン）は、2011年7月に発生し、複雑な動きをした台風である。この台風は統計史上7月最強級の勢力となっており、8月12日の閣議において、局地激甚災害に指定された。
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태풍 망온(태풍 번호: 1106, JTWC 지정 번호: 08W, 국제명:MA-ON, 필리핀 기상청(PAGASA) 지정 이름: Ineng)는 2011년 북서태평양에서 발생한 6번째 태풍으로, 태풍의 직접 영향을 받았던 일본에 막대한 피해를 냈다. “망온”은 홍콩에서 제출한 이름으로 '말안장'을 의미한다.
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颱風馬鞍（英語：Typhoon Ma-on），在菲律賓被稱為颱風伊能，是個規模龐大且風力強勁的颱風，在2011年7月影響日本南部。它是2011年太平洋颱風季的第六個獲得命名的風暴和第二個颱風。馬鞍的前身起源於7月9日一個位於威克島附近的低氣壓區，隨著它向西移動並逐漸。到7月11日，其組織已經有足夠改善，可以被宣佈成為熱帶低氣壓，然而氣旋的環流仍然廣闊。在接下來的幾天裏，馬鞍逐漸增強，並在7月14日達到颱風的標準。有利的環境條件使其進一步增強，風暴最終在7月16日達到最高十分鐘持續風速每小時175公里/小時。在副熱帶高壓脊減弱後，颱風轉向北方，並經歷一系列導致其減弱的眼牆置換循環。7月19日，馬鞍吹襲四國，然後轉向東南方並返回海面。隨著馬鞍受強烈的风切变影響，繼續緩慢地減弱。該系統最終在7月24日轉變成溫帶氣旋，日本氣象廳在一周後於堪察加半島附近最後一次標注該系統。 最初，馬鞍對馬里亞納群島構成輕微威脅並促使當局發佈熱帶風暴警告。然而，該系統在該區較遠處掠過，僅產生零星降雨。在日本，數百人從泥石流多發地區撤離。風暴產生的暴雨估計超過1,200毫米，引發大範圍具破壞性的水災。馬鞍造成五人死亡，損失達到39億日圓（5000萬美元，2011年）。
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Typhoon Ma-on, known in the Philippines as Typhoon Ineng, was a large and powerful typhoon that affected southern Japan in July 2011. It was the sixth named storm and second typhoon of the 2011 Pacific typhoon season. Originating from an area of low pressure near Wake Island on July 9, the precursor to Ma-on gradually developed as it moved westward. By July 11, it had become sufficiently organized to be declared a tropical depression, although the cyclone's circulation remained broad. Over the following days, Ma-on gradually intensified and attained typhoon status on July 14. Favorable environmental conditions allowed for additional strengthening, and the storm ultimately attained peak ten-minute sustained winds of 175 km/h (110 mph) on July 16. After turning northward in response to a wea
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태풍 망온 (2011년)
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平成23年台風第6号
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Typhoon Ma-on (2011)
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颱風馬鞍 (2011年)
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Typhoon Ma-on
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115
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WPac
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2011-07-31
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--07-24
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2011
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50
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5
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2011-07-11
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Typhoon Ma-on Jul 16 2011 0145Z.jpg
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Typhoon Ma-on near peak intensity on July 16
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935
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typhoon
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2011
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95
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135
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Typhoon Ma-on, known in the Philippines as Typhoon Ineng, was a large and powerful typhoon that affected southern Japan in July 2011. It was the sixth named storm and second typhoon of the 2011 Pacific typhoon season. Originating from an area of low pressure near Wake Island on July 9, the precursor to Ma-on gradually developed as it moved westward. By July 11, it had become sufficiently organized to be declared a tropical depression, although the cyclone's circulation remained broad. Over the following days, Ma-on gradually intensified and attained typhoon status on July 14. Favorable environmental conditions allowed for additional strengthening, and the storm ultimately attained peak ten-minute sustained winds of 175 km/h (110 mph) on July 16. After turning northward in response to a weakening subtropical ridge, the typhoon underwent a series of eyewall replacement cycles that caused it to weaken. On July 19, Ma-on struck Shikoku before turning southeastward and moving back over water. Slow weakening continued as Ma-on succumbed to the effects of high wind shear. The system ultimately became extratropical on July 24, and was last noted by the Japan Meteorological Agency a week later near the Kamchatka Peninsula. Initially, Ma-on posed a slight threat to the Mariana Islands and prompted the issuance of tropical storm warnings. However, the system remained far away from the area and only produced scattered rainfall. In Japan, hundreds of people evacuated from mudslide-prone areas. Torrential rains produced by the storm, estimated at more than 1,200 mm (48 in), led to widespread and damaging floods. Five people perished as a result of Ma-on, and damage reached ¥3.9 billion (2011 JPY, $50 million 2011 USD).
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平成23年台風第6号（へいせい23ねんたいふうだい6ごう、アジア名：マーゴン）は、2011年7月に発生し、複雑な動きをした台風である。この台風は統計史上7月最強級の勢力となっており、8月12日の閣議において、局地激甚災害に指定された。
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태풍 망온(태풍 번호: 1106, JTWC 지정 번호: 08W, 국제명:MA-ON, 필리핀 기상청(PAGASA) 지정 이름: Ineng)는 2011년 북서태평양에서 발생한 6번째 태풍으로, 태풍의 직접 영향을 받았던 일본에 막대한 피해를 냈다. “망온”은 홍콩에서 제출한 이름으로 '말안장'을 의미한다.
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颱風馬鞍（英語：Typhoon Ma-on），在菲律賓被稱為颱風伊能，是個規模龐大且風力強勁的颱風，在2011年7月影響日本南部。它是2011年太平洋颱風季的第六個獲得命名的風暴和第二個颱風。馬鞍的前身起源於7月9日一個位於威克島附近的低氣壓區，隨著它向西移動並逐漸。到7月11日，其組織已經有足夠改善，可以被宣佈成為熱帶低氣壓，然而氣旋的環流仍然廣闊。在接下來的幾天裏，馬鞍逐漸增強，並在7月14日達到颱風的標準。有利的環境條件使其進一步增強，風暴最終在7月16日達到最高十分鐘持續風速每小時175公里/小時。在副熱帶高壓脊減弱後，颱風轉向北方，並經歷一系列導致其減弱的眼牆置換循環。7月19日，馬鞍吹襲四國，然後轉向東南方並返回海面。隨著馬鞍受強烈的风切变影響，繼續緩慢地減弱。該系統最終在7月24日轉變成溫帶氣旋，日本氣象廳在一周後於堪察加半島附近最後一次標注該系統。 最初，馬鞍對馬里亞納群島構成輕微威脅並促使當局發佈熱帶風暴警告。然而，該系統在該區較遠處掠過，僅產生零星降雨。在日本，數百人從泥石流多發地區撤離。風暴產生的暴雨估計超過1,200毫米，引發大範圍具破壞性的水災。馬鞍造成五人死亡，損失達到39億日圓（5000萬美元，2011年）。
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26749
