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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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