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  Will greenhouse gas-induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes?

Bengtsson, L., Botzet, M., & Esch, M. (1996). Will greenhouse gas-induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes? Tellus, Series A: Dynamic Meteorology and Oceanography, 48, 57-73. doi:10.3402/tellusa.v48i1.11632.

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アイテムのパーマリンク: https://hdl.handle.net/21.11116/0000-000B-1B6B-0 版のパーマリンク: https://hdl.handle.net/21.11116/0000-000B-1CF7-0
資料種別: 学術論文

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Will greenhouse gas induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes.pdf (出版社版), 4MB
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https://hdl.handle.net/21.11116/0000-000B-1B6D-E
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Will greenhouse gas induced warming over the next 50 years lead to higher frequency and greater intensity of hurricanes.pdf
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 作成者:
Bengtsson, Lennart1, 著者           
Botzet, Michael1, 著者           
Esch, Monika1, 著者           
所属:
1MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913545              

内容説明

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キーワード: Frequency/Intensity; Global Warming; Greenhouse Effect; Hurricanes, carbon dioxide doubling; climate change; climate exchange experiment; global warming; greenhouse gas; high resolution atmospheric modelling; hurricane genesis; hurricanes; model; storm climatology; tropical storm climatology
 要旨: The use of a high resolution atmospheric model at T106 resolution, for studying the influence of greenhouse warming on tropical storm climatology, is investigated. The same method for identifying the storms has been used as in a previous study by Bengtsson et al. The sea surface temperature anomalies have been taken from a previous transient climate change experiment, obtained with a low resolution ocean-atmosphere coupled model. The global distribution of the storms, at the time when the CO2 concentration in the atmosphere had doubled, agrees in geographical position and seasonal variability with that of the present climate, but the number of storms is significantly reduced, particularly at the Southern Hemisphere. The main reason to this, appear to be connected to changes in the large scale circulation, such as a weaker Hadley circulation and stronger upper air westerlies. The low level vorticity in the hurricane genesis regions is generally reduced compared to the present climate, while the vertical tropospheric wind shear is somewhat increased. Most tropical storm regions indicate reduced surface windspeeds and a slightly weaker hydrological cycle.

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言語: eng - English
 日付: 1996
 出版の状態: 出版
 ページ: -
 出版情報: -
 目次: -
 査読: 査読あり
 識別子(DOI, ISBNなど): DOI: 10.3402/tellusa.v48i1.11632
BibTex参照ID: Bengtsson199657
 学位: -

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出版物 1

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出版物名: Tellus, Series A: Dynamic Meteorology and Oceanography
種別: 学術雑誌
 著者・編者:
所属:
出版社, 出版地: Blackwell Munksgaard
ページ: - 巻号: 48 通巻号: - 開始・終了ページ: 57 - 73 識別子(ISBN, ISSN, DOIなど): ISSN: 02806495