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    Future Changes in Tropical Cyclone Activity Projected by the New High-Resolution MRI-AGCM

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 009::page 3237
    Author:
    Murakami, Hiroyuki
    ,
    Wang, Yuqing
    ,
    Yoshimura, Hiromasa
    ,
    Mizuta, Ryo
    ,
    Sugi, Masato
    ,
    Shindo, Eiki
    ,
    Adachi, Yukimasa
    ,
    Yukimoto, Seiji
    ,
    Hosaka, Masahiro
    ,
    Kusunoki, Shoji
    ,
    Ose, Tomoaki
    ,
    Kitoh, Akio
    DOI: 10.1175/JCLI-D-11-00415.1
    Publisher: American Meteorological Society
    Abstract: ew versions of the high-resolution 20- and 60-km-mesh Meteorological Research Institute (MRI) atmospheric general circulation models (MRI-AGCM version 3.2) have been developed and used to investigate potential future changes in tropical cyclone (TC) activity. Compared with the previous version (version 3.1), version 3.2 yields a more realistic simulation of the present-day (1979?2003) global distribution of TCs. Moreover, the 20-km-mesh model version 3.2 is able to simulate extremely intense TCs (categories 4 and 5), which is the first time a global climate model has been able to simulate such extremely intense TCs through a multidecadal simulation. Future (2075?99) projections under the Intergovernmental Panel on Climate Change (IPCC) A1B scenario are conducted using versions 3.1 and 3.2, showing consistent decreases in the number of TCs globally and in both hemispheres as climate warms. Although projected future changes in basin-scale TC numbers show some differences between the two versions, the projected frequency of TC occurrence shows a consistent decrease in the western part of the western North Pacific (WNP) and in the South Pacific Ocean (SPO), while it shows a marked increase in the central Pacific. Both versions project a future increase in the frequency of intense TCs globally; however, the degree of increase is smaller in version 3.2 than in version 3.1. This difference arises partly because version 3.2 projects a pronounced decrease in mean TC intensity in the SPO. The 20-km-mesh model version 3.2 projects a northward shift in the most intense TCs (category 5) in the WNP, indicating an increasing potential for future catastrophic damage due to TCs in this region.
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      Future Changes in Tropical Cyclone Activity Projected by the New High-Resolution MRI-AGCM

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221848
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    • Journal of Climate

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    contributor authorMurakami, Hiroyuki
    contributor authorWang, Yuqing
    contributor authorYoshimura, Hiromasa
    contributor authorMizuta, Ryo
    contributor authorSugi, Masato
    contributor authorShindo, Eiki
    contributor authorAdachi, Yukimasa
    contributor authorYukimoto, Seiji
    contributor authorHosaka, Masahiro
    contributor authorKusunoki, Shoji
    contributor authorOse, Tomoaki
    contributor authorKitoh, Akio
    date accessioned2017-06-09T17:04:57Z
    date available2017-06-09T17:04:57Z
    date copyright2012/05/01
    date issued2011
    identifier issn0894-8755
    identifier otherams-79104.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221848
    description abstractew versions of the high-resolution 20- and 60-km-mesh Meteorological Research Institute (MRI) atmospheric general circulation models (MRI-AGCM version 3.2) have been developed and used to investigate potential future changes in tropical cyclone (TC) activity. Compared with the previous version (version 3.1), version 3.2 yields a more realistic simulation of the present-day (1979?2003) global distribution of TCs. Moreover, the 20-km-mesh model version 3.2 is able to simulate extremely intense TCs (categories 4 and 5), which is the first time a global climate model has been able to simulate such extremely intense TCs through a multidecadal simulation. Future (2075?99) projections under the Intergovernmental Panel on Climate Change (IPCC) A1B scenario are conducted using versions 3.1 and 3.2, showing consistent decreases in the number of TCs globally and in both hemispheres as climate warms. Although projected future changes in basin-scale TC numbers show some differences between the two versions, the projected frequency of TC occurrence shows a consistent decrease in the western part of the western North Pacific (WNP) and in the South Pacific Ocean (SPO), while it shows a marked increase in the central Pacific. Both versions project a future increase in the frequency of intense TCs globally; however, the degree of increase is smaller in version 3.2 than in version 3.1. This difference arises partly because version 3.2 projects a pronounced decrease in mean TC intensity in the SPO. The 20-km-mesh model version 3.2 projects a northward shift in the most intense TCs (category 5) in the WNP, indicating an increasing potential for future catastrophic damage due to TCs in this region.
    publisherAmerican Meteorological Society
    titleFuture Changes in Tropical Cyclone Activity Projected by the New High-Resolution MRI-AGCM
    typeJournal Paper
    journal volume25
    journal issue9
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00415.1
    journal fristpage3237
    journal lastpage3260
    treeJournal of Climate:;2011:;volume( 025 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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