Mamalakis Antonios, Randerson James T, Yu Jin-Yi, Pritchard Michael S, Magnusdottir Gudrun, Smyth Padhraic, Levine Paul A, Yu Sungduk, Foufoula-Georgiou Efi
Department of Civil and Environmental Engineering, University of California, Irvine.
Department of Earth System Science, University of California, Irvine.
Nat Clim Chang. 2021 Feb 1;11:143-151. doi: 10.1038/s41558-020-00963-x. Epub 2021 Jan 18.
Future changes in the position of the intertropical convergence zone (ITCZ; a narrow band of heavy precipitation in the tropics) with climate change could affect the livelihood and food security of billions of people. Although models predict a future narrowing of the ITCZ, uncertainties remain large regarding its future position, with most past work focusing on zonal-mean shifts. Here we use projections from 27 state-of-the-art (CMIP6) climate models and document a robust zonally-varying ITCZ response to the SSP3-7.0 scenario by 2100, with a northward shift over eastern Africa and the Indian Ocean, and a southward shift in the eastern Pacific and Atlantic Oceans. The zonally-varying response is consistent with changes in the divergent atmospheric energy transport, and sector-mean shifts of the energy flux equator. Our analysis provides insight about mechanisms influencing the future position of the tropical rainbelt, and may allow for more robust projections of climate change impacts.
热带辐合带(ITCZ;热带地区一条狭窄的强降水带)的位置随气候变化的未来变化可能会影响数十亿人的生计和粮食安全。尽管模型预测ITCZ未来会变窄,但其未来位置的不确定性仍然很大,过去的大多数研究都集中在纬向平均移动上。在这里,我们使用了27个最先进的(CMIP6)气候模型的预测,并记录了到2100年ITCZ对SSP3-7.0情景的一种稳健的纬向变化响应,即非洲东部和印度洋上空向北移动,而东太平洋和大西洋上空向南移动。这种纬向变化响应与发散的大气能量传输变化以及能量通量赤道的区域平均移动一致。我们的分析提供了关于影响热带雨带未来位置机制的见解,并可能有助于对气候变化影响进行更可靠的预测。