Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195-1640, USA.
Proc Natl Acad Sci U S A. 2013 Mar 26;110(13):4935-40. doi: 10.1073/pnas.1213302110. Epub 2013 Mar 14.
The double-Intertropical Convergence Zone (ITCZ) problem, in which excessive precipitation is produced in the Southern Hemisphere tropics, which resembles a Southern Hemisphere counterpart to the strong Northern Hemisphere ITCZ, is perhaps the most significant and most persistent bias of global climate models. In this study, we look to the extratropics for possible causes of the double-ITCZ problem by performing a global energetic analysis with historical simulations from a suite of global climate models and comparing with satellite observations of the Earth's energy budget. Our results show that models with more energy flux into the Southern Hemisphere atmosphere (at the top of the atmosphere and at the surface) tend to have a stronger double-ITCZ bias, consistent with recent theoretical studies that suggest that the ITCZ is drawn toward heating even outside the tropics. In particular, we find that cloud biases over the Southern Ocean explain most of the model-to-model differences in the amount of excessive precipitation in Southern Hemisphere tropics, and are suggested to be responsible for this aspect of the double-ITCZ problem in most global climate models.
热带辐合带(ITCZ)双带问题,即在南半球热带地区产生过度降水,类似于北半球强 ITCZ 的南半球对应现象,可能是全球气候模型最显著和最持久的偏差。在这项研究中,我们通过对一系列全球气候模型的历史模拟进行全球能量分析,并与地球能量收支的卫星观测进行比较,从亚热带地区寻找双 ITCZ 问题的可能原因。我们的结果表明,具有更多能量流入南半球大气(在平流层顶和地表)的模型往往具有更强的双 ITCZ 偏差,这与最近的理论研究一致,即 ITCZ 被吸引到热带以外的加热区。特别是,我们发现南大洋上空的云偏差解释了南半球热带地区过量降水模型间的大部分差异,并被认为是大多数全球气候模型中双 ITCZ 问题的这一方面的原因。