Modification of cirrus clouds to reduce global warming

被引:112
作者
Mitchell, David L. [1 ]
Finnegan, William [1 ]
机构
[1] Desert Res Inst, Reno, NV 89512 USA
来源
ENVIRONMENTAL RESEARCH LETTERS | 2009年 / 4卷 / 04期
关键词
geoengineering; cirrus clouds; climate modeling; HOMOGENEOUS ICE NUCLEATION; RELATIVE-HUMIDITY; AEROSOLS; PARTICLES; NUCLEI; WATER;
D O I
10.1088/1748-9326/4/4/045102
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Greenhouse gases and cirrus clouds regulate outgoing longwave radiation (OLR) and cirrus cloud coverage is predicted to be sensitive to the ice fall speed which depends on ice crystal size. The higher the cirrus, the greater their impact is on OLR. Thus by changing ice crystal size in the coldest cirrus, OLR and climate might be modified. Fortunately the coldest cirrus have the highest ice supersaturation due to the dominance of homogeneous freezing nucleation. Seeding such cirrus with very efficient heterogeneous ice nuclei should produce larger ice crystals due to vapor competition effects, thus increasing OLR and surface cooling. Preliminary estimates of this global net cloud forcing are more negative than -2.8 W m(-2) and could neutralize the radiative forcing due to a CO2 doubling (3.7 W m(-2)). A potential delivery mechanism for the seeding material is already in place: the airline industry. Since seeding aerosol residence times in the troposphere are relatively short, the climate might return to its normal state within months after stopping the geoengineering experiment. The main known drawback to this approach is that it would not stop ocean acidification. It does not have many of the drawbacks that stratospheric injection of sulfur species has.
引用
收藏
页数:8
相关论文
共 54 条
[1]   Testing an ensemble model of cirrus ice crystals using midlatitude in situ estimates of ice water content, volume extinction coefficient and the total solar optical depth [J].
Baran, Anthony J. ;
Connolly, P. J. ;
Lee, C. .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2009, 110 (14-16) :1579-1598
[2]   Storm tracks and climate change [J].
Bengtsson, Lennart ;
Hodges, Kevin I. ;
Roeckner, Erich .
JOURNAL OF CLIMATE, 2006, 19 (15) :3518-3543
[3]  
Chen T, 2000, J CLIMATE, V13, P264, DOI 10.1175/1520-0442(2000)013<0264:REOCTV>2.0.CO
[4]  
2
[5]   Aerosol indirect effect over the Indian Ocean [J].
Chylek, P ;
Dubey, MK ;
Lohmann, U ;
Ramanathan, V ;
Kaufman, YJ ;
Lesins, G ;
Hudson, J ;
Altmann, G ;
Olsen, S .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (06)
[6]  
Cotton WR, 2009, CLOUDS IN THE PERTURBED CLIMATE SYSTEM: THEIR RELATIONSHIP TO ENERGY BALANCE, ATMOSPHERIC DYNAMICS, AND PRECIPITATION, P339
[7]  
DeMott P.J., 2002, Cirrus: Laboratory Studies of Cirrus Cloud Processes, P102
[8]   Ice formation by black carbon particles [J].
DeMott, PJ ;
Chen, Y ;
Kreidenweis, SM ;
Rogers, DC ;
Sherman, DE .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (16) :2429-2432
[9]   The susceptibility of ice formation in upper tropospheric clouds to insoluble aerosol components [J].
DeMott, PJ ;
Rogers, DC ;
Kreidenweis, SM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D16) :19575-19584
[10]   African dust aerosols as atmospheric ice nuclei [J].
DeMott, PJ ;
Sassen, K ;
Poellot, MR ;
Baumgardner, D ;
Rogers, DC ;
Brooks, SD ;
Prenni, AJ ;
Kreidenweis, SM .
GEOPHYSICAL RESEARCH LETTERS, 2003, 30 (14) :ASC1-1