Weakening of hurricanes via marine cloud brightening (MCB)

被引:20
|
作者
Latham, John [2 ,3 ]
Parkes, Ben
Gadian, Alan [1 ]
Salter, Stephen [4 ]
机构
[1] Univ Leeds, Dept Environm, SEE, NCAS, Leeds LS2 9JT, W Yorkshire, England
[2] Natl Ctr Atmospher Res, MMM Div, Boulder, CO 80307 USA
[3] Univ Manchester, SEAS, Manchester M13 9PL, Lancs, England
[4] Univ Edinburgh, Dept Engn, Edinburgh EH8 9YL, Midlothian, Scotland
来源
ATMOSPHERIC SCIENCE LETTERS | 2012年 / 13卷 / 04期
关键词
hurricanes; marine cloud brightening; sea surface temperature; cloud seeding; global climate modelling; LEVEL MARITIME CLOUDS; TROPICAL CYCLONES; POTENTIAL INTENSITY; ATLANTIC HURRICANES; ALBEDO-ENHANCEMENT; FREQUENCY; MICROPHYSICS; TEMPERATURE; MODEL;
D O I
10.1002/asl.402
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper examines the potential to cool ocean surface waters in regions of hurricane genesis and early development. This would be achieved by seeding, with copious quantities of seawater cloud condensation nuclei (CCN), low-level maritime stratocumulus clouds covering these regions or those at the source of incoming currents. Higher cloud droplet density would increase these clouds' reflectivity to incoming sunlight, and possibly their longevity. This approach is therefore a more localized application of the marine cloud brightening (MCB) geoengineering technique promoting global cooling. By utilizing a climate ocean/atmosphere coupled model, HadGEM1, we demonstrate thatsubject to the satisfactory resolution of defined but unresolved issuesjudicious seeding of maritime stratocumulus clouds might significantly reduce sea surface temperatures (SSTs) in regions where hurricanes develop. Thus artificial seeding may reduce hurricane intensity; but how well the magnitude of this effect could be controlled is yet to be determined. We also address the important question as to how MCB seeding may influence precipitation. GCM modelling indicates that the influence of seeding on undesirable rainfall reductions depends on its location and magnitude. Much more work on this topic is required. Copyright (c) 2012 Royal Meteorological Society
引用
收藏
页码:231 / 237
页数:7
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