Duffy Grant A, Montiel Fabien, Purich Ariaan, Fraser Ceridwen I
Department of Marine Science, University of Otago, Dunedin 9054, New Zealand.
Department of Mathematics and Statistics, University of Otago, Dunedin 9054, New Zealand.
Proc Natl Acad Sci U S A. 2024 Mar 12;121(11):e2321595121. doi: 10.1073/pnas.2321595121. Epub 2024 Mar 4.
Polynyas, areas of open water embedded within sea ice, are a key component of ocean-atmosphere interactions that act as hotspots of sea-ice production, bottom-water formation, and primary productivity. The specific drivers of polynya dynamics remain, however, elusive and coupled climate models struggle to replicate Antarctic polynya activity. Here, we leverage a 44-y time series of Antarctic sea ice to elucidate long-term trends. We identify Antarctic-wide linear increases and a hitherto undescribed cyclical pattern of polynya activity across the Ross Sea region that potentially arises from interactions between the Amundsen Sea Low and Southern Annular Mode. While their specific drivers remain unknown, identifying these emerging patterns augments our capacity to understand the processes that influence sea ice. As we enter a potentially new age of Antarctic sea ice, this advance in understanding will, in turn, lead to more accurate predictions of environmental change, and its implications for Antarctic ecosystems.
冰间湖是嵌入海冰中的开阔水域,是海气相互作用的关键组成部分,充当着海冰生成、底层水形成和初级生产力的热点区域。然而,冰间湖动态变化的具体驱动因素仍然难以捉摸,耦合气候模型也难以复制南极冰间湖活动。在此,我们利用长达44年的南极海冰时间序列来阐明长期趋势。我们识别出整个南极范围内冰间湖活动呈线性增加,以及罗斯海地区一种迄今未被描述的周期性模式,这种模式可能源于阿蒙森海低压和南半球环状模之间的相互作用。虽然其具体驱动因素仍然未知,但识别出这些新出现的模式增强了我们理解影响海冰过程的能力。随着我们进入一个南极海冰的潜在新时代,这种理解上的进步反过来将带来对环境变化及其对南极生态系统影响的更准确预测。