翻訳と辞書
Words near each other
・ Cyclone Innis
・ Cyclone Isobel
・ Cyclone Ita
・ Cyclone Ivan
・ Cyclone Ivy
・ Cyclone Jal
・ Cyclone Japhet
・ Cyclone Jasmine
・ Cyclone Jeanett
・ Cyclone Joachim
・ Cyclone Joan
・ Cyclone Joe Williams
・ Cyclone John
・ Cyclone Jokwe
・ Cyclone Joy
Cyclone Justin
・ Cyclone Kalunde
・ Cyclone Kamba
・ Cyclone Kamisy
・ Cyclone Kate (2006)
・ Cyclone Kathy
・ Cyclone Katrina
・ Cyclone Keila
・ Cyclone Keli
・ Cyclone Kesiny
・ Cyclone Kina
・ Cyclone Klaus
・ Cyclone Laila
・ Cyclone Lake
・ Cyclone Lam


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Cyclone Justin : ウィキペディア英語版
Cyclone Justin

Cyclone Justin was a tropical cyclone of the 1996-97 Southern Hemisphere tropical cyclone season that caused seven deaths and had a major economic impact in northern Queensland, Australia. It had a long 3½-week life from 3 March to 29 March 1997. Peaking as a Category 4 cyclone and making landfall as a Category 2, it caused significant damage in the Cairns region, which it approached on two occasions. Houses were undermined by huge waves, a marina and boats were severely damaged, roads and bridges suffered from flood and landslide damage and huge losses were inflicted on sugar cane, fruit and vegetable crops. The death toll in Queensland was seven including five on a yacht which sank. There were 26 who died in Papua New Guinea, which was also severely affected. Total estimated costs from damages in Australia were $190 million (1997 values).
==Meteorological history==

On 3 March 1997 the Australian Bureau of Meteorology (BoM) observed two areas of low pressure, that had developed within the monsoon trough from North-eastern Australia to the Coral Sea. Over the next couple of days, both systems developed further and were classified as tropical depressions during 5 March.
On 7 March, over the Coral Sea, Cyclone Justin began to form. The way in which it formed was as follows. The sea waters were at least 27 °C, and as a result some of this water was evaporated into the air. This water vapour then rose upwards and created large cumulonimbus clouds. These clouds grouped together and caused a current of warm, moist, rapidly rising air to occur. As a result of this current a low-pressure area on the surface of the sea began to develop. This low-pressure area made the trade winds (In the southern hemisphere, where Cyclone Justin formed, they are the east to south-easterly winds) to become much stronger, and indeed, allowed them to impart enough force to rotate the cumulonimbus clouds. As these winds spiralled around the low-pressure area (the ‘eye’) they released heat and moisture which supplied the now cyclone with energy.
It spent the first week of its life following an erratic path around the Coral Sea; however, with the constant cloud cover the water temperature dropped 4 °C. As a consequence of this, Cyclone Justin was deprived of its vital energy source (the warm water vapour) and therefore moved northeast, towards Papua New Guinea to warmer water. Here, it grew to a Category 3 cyclone and caused storm force winds and storm surges. On 22 March it retreated to Queensland where it made landfall, as a Category 2 cyclone, north of Cairns. The areas in and around Cairns, Innisfail and Mareeba areas were devastated with large storm surges, excessive flooding, gusts of winds which reached up to 130 km/h and landslides.

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「Cyclone Justin」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.