Hadley Cell Widening: Model Simulations versus Observations

被引:253
作者
Johanson, Celeste M. [1 ]
Fu, Qiang [1 ]
机构
[1] Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA
关键词
METEOROLOGICAL REGIMES; CLIMATE; CIRCULATION; PERTURBATIONS; ATMOSPHERE;
D O I
10.1175/2008JCLI2620.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Observations show that the Hadley cell has widened by about 2 degrees-5 degrees since 1979. This widening and the concomitant poleward displacement of the subtropical dry zones may be accompanied by large-scale drying near 30 degrees N and 30 degrees S. Such drying poses a risk to inhabitants of these regions who are accustomed to established rainfall patterns. Simple and comprehensive general circulation models (GCMs) indicate that the Hadley cell may widen in response to global warming, warming of the west Pacific, or polar stratospheric cooling. The combination of these factors may be responsible for the recent observations. But there is no study so far that has compared the observed widening to GCM simulations of twentieth-century climate integrated with historical changes in forcings. Here the Hadley cell widening is assessed in current GCMs from historical simulations of the twentieth century as well as future climate projections and preindustrial control runs. The authors find that observed widening cannot be explained by natural variability. This observed widening is also significantly larger than in simulations of the twentieth and twenty-first centuries. These results illustrate the need for further investigation into the discrepancy between the observed and simulated widening of the Hadley cell.
引用
收藏
页码:2713 / 2725
页数:13
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