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

被引:313
作者
Murakami, Hiroyuki [1 ]
Wang, Yuqing [2 ,3 ]
Yoshimura, Hiromasa
Mizuta, Ryo
Sugi, Masato
Shindo, Eiki
Adachi, Yukimasa
Yukimoto, Seiji
Hosaka, Masahiro
Kusunoki, Shoji
Ose, Tomoaki
Kitoh, Akio
机构
[1] Japan Agcy Marine Earth Sci & Technol, Meteorol Res Inst, JAMSTEC, Tsukuba, Ibaraki 3050052, Japan
[2] Univ Hawaii Manoa, Dept Meteorol, Honolulu, HI 96822 USA
[3] Univ Hawaii Manoa, Int Pacific Res Ctr, Honolulu, HI 96822 USA
基金
美国国家科学基金会;
关键词
INTRASEASONAL VARIABILITY; POTENTIAL INTENSITY; CLIMATE; MODEL; HURRICANE; FREQUENCY; SIMULATIONS; PACIFIC; IMPACT;
D O I
10.1175/JCLI-D-11-00415.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
New 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.
引用
收藏
页码:3237 / 3260
页数:24
相关论文
共 71 条
  • [1] Ice-sheet mass balance: assessment, attribution and prognosis
    Alley, Richard B.
    Spencer, Matthew K.
    Anandakrishnan, Sridhar
    [J]. ANNALS OF GLACIOLOGY, VOL 46, 2007, 2007, 46 : 1 - +
  • [2] [Anonymous], UN WEATH HURR TROP D
  • [3] [Anonymous], 2008, ESTIMATION FUTURE DI
  • [4] ARAKAWA A, 1974, J ATMOS SCI, V31, P674, DOI 10.1175/1520-0469(1974)031<0674:IOACCE>2.0.CO
  • [5] 2
  • [6] ATKINSON GD, 1977, MON WEATHER REV, V105, P421, DOI 10.1175/1520-0493(1977)105<0421:TCMSLP>2.0.CO
  • [7] 2
  • [8] 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
    [J]. TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 1996, 48 (01) : 57 - 73
  • [9] How may tropical cyclones change in a warmer climate?
    Bengtsson, Lennart
    Hodges, Kevin I.
    Esch, Monika
    Keenlyside, Noel
    Kornblueh, Luis
    Luo, Jing-Jia
    Yamagata, Toshio
    [J]. TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2007, 59 (04) : 539 - 561
  • [10] Dissipative heating and hurricane intensity
    Bister, M
    Emanuel, KA
    [J]. METEOROLOGY AND ATMOSPHERIC PHYSICS, 1998, 65 (3-4) : 233 - 240