MODELING SEA-SURFACE TEMPERATURE RISE RESULTING FROM INCREASING ATMOSPHERIC CARBON-DIOXIDE CONCENTRATIONS

被引:7
作者
HENDERSONSELLERS, B
机构
[1] Univ of Salford, Salford, Engl, Univ of Salford, Salford, Engl
关键词
ATMOSPHERIC COMPOSITION - CARBON DIOXIDE - Environmental Impact - METEOROLOGY - Climatology;
D O I
10.1007/BF00143324
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Concern over the role of the oceans in a warming world, likely to result from increasing atmospheric carbon dioxide, has prompted analysis using simple models. Results from two recent, independent studies using a simple box-diffusion model suggest that over the last 130 years, observations and models are not in disagreement. Although a diffusive deep ocean was indeed included in this simplistic model, it is suggested here that the resulting ocean model offers an oversimplistic view of the oceanic contribution to the overall global atmosphere-ocean climate system and that it is necessary to add a convective capability to the water column. Using this approach it is suggested that, on a timescale of a century, the sea surface temperature increase is likely to be less by a factor of at least 3 than that previously forecast.
引用
收藏
页码:349 / 359
页数:11
相关论文
共 30 条
[1]  
Brutsaert W., 1982, EVAPORATION ATMOSPHE
[2]  
BRYAN K, 1984, CLIMATE PROCESSES CL, P29
[3]  
DICKINSON RE, 1985, ADV GEOPHYS, V28, P99
[4]   WORLDWIDE MARINE TEMPERATURE-FLUCTUATIONS 1856-1981 [J].
FOLLAND, CK ;
PARKER, DE ;
KATES, FE .
NATURE, 1984, 310 (5979) :670-673
[5]   COMPARISON OF SEASONAL THERMOCLINE MODELS WITH OBSERVATION [J].
GILL, AE ;
TURNER, JS .
DEEP-SEA RESEARCH, 1976, 23 (05) :391-401
[6]  
HANEY RL, 1976, J PHYS OCEANOGR, V6, P504, DOI 10.1175/1520-0485(1976)006<0504:TROSMI>2.0.CO
[7]  
2
[8]   CLIMATE RESPONSE-TIMES - DEPENDENCE ON CLIMATE SENSITIVITY AND OCEAN MIXING [J].
HANSEN, J ;
RUSSELL, G ;
LACIS, A ;
FUNG, I ;
RIND, D ;
STONE, P .
SCIENCE, 1985, 229 (4716) :857-859
[9]  
Hansen J., 1984, CLIMATE PROCESSES CL, P130, DOI [10.1029/GM029p0130, DOI 10.1029/GM029P0130]
[10]   TRANSIENT CLIMATE RESPONSE TO EXTERNAL FORCING ON 10(0)-10(4) YEAR TIME SCALES .1. EXPERIMENTS WITH GLOBALLY AVERAGED, COUPLED, ATMOSPHERE AND OCEAN ENERGY-BALANCE MODELS [J].
HARVEY, LDD ;
SCHNEIDER, SH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1985, 90 (ND1) :2191-2205