Tropical Cyclones and Climate Change Assessment: Part II: Projected Response to Anthropogenic Warming

被引:630
|
作者
Knutson, Thomas [1 ]
Camargo, Suzana J. [2 ]
Chan, Johnny C. L. [3 ]
Emanuel, Kerry [4 ]
Ho, Chang-Hoi [5 ]
Kossin, James [6 ]
Mohapatra, Mrutyunjay [7 ]
Satoh, Masaki [8 ]
Sugi, Masato [9 ]
Walsh, Kevin [10 ]
Wu, Liguang [11 ]
机构
[1] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
[3] City Univ Hong Kong, Guy Carpenter Asia Pacific Climate Impact Ctr, Kowloon, Hong Kong, Peoples R China
[4] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
[5] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul, South Korea
[6] NOAA, Natl Ctr Environm Informat, Ctr Weather & Climate, Madison, WI USA
[7] Indian Meteorol Dept, New Delhi, India
[8] Univ Tokyo, Atmosphere & Ocean Res Inst, Chiba, Japan
[9] Meteorol Res Inst, Tsukuba, Ibaraki, Japan
[10] Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia
[11] Nanjing Univ Informat Sci & Technol, Nanjing, Jiangsu, Peoples R China
关键词
WESTERN NORTH PACIFIC; NEW-YORK-CITY; SEA-LEVEL; FUTURE CHANGES; HURRICANE INTENSITY; COUPLED MODEL; RESOLUTION; SIMULATIONS; FREQUENCY; IMPACT;
D O I
10.1175/BAMS-D-18-0194.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Model projections of tropical cyclone (TC) activity response to anthropogenic warming in climate models are assessed. Observations, theory, and models, with increasing robustness, indicate rising global TC risk for some metrics that are projected to impact multiple regions. A 2 degrees C anthropogenic global warming is projected to impact TC activity as follows. 1) The most confident TC-related projection is that sea level rise accompanying the warming will lead to higher storm inundation levels, assuming all other factors are unchanged. 2) For TC precipitation rates, there is at least medium-to-high confidence in an increase globally, with a median projected increase of 14%, or close to the rate of tropical water vapor increase with warming, at constant relative humidity. 3) For TC intensity, 10 of 11 authors had at least medium-to-high confidence that the global average will increase. The median projected increase in lifetime maximum surface wind speeds is about 5% (range: 1%-10%) in available higher-resolution studies. 4) For the global proportion (as opposed to frequency) of TCs that reach very intense (category 4-5) levels, there is at least medium-to-high confidence in an increase, with a median projected change of +13%. Author opinion was more mixed and confidence levels lower for the following projections: 5) a further poleward expansion of the latitude of maximum TC intensity in the western North Pacific; 6) a decrease of global TC frequency, as projected in most studies; 7) an increase in global very intense TC frequency (category 4-5), seen most prominently in higher-resolution models; and 8) a slowdown in TC translation speed.
引用
收藏
页码:E303 / E322
页数:20
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