气候变化中的极地海洋和海冰

IF 4.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Megan D. Willis, Delphine Lannuzel, Brent Else, Hélène Angot, Karley Campbell, Odile Crabeck, Bruno Delille, Hakase Hayashida, Martine Lizotte, Brice Loose, Klaus M. Meiners, Lisa Miller, Sebastien Moreau, Daiki Nomura, John Prytherch, Julia Schmale, Nadja Steiner, Letizia Tedesco, Jennie Thomas
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引用次数: 3

摘要

极地海洋和海冰覆盖了地球海洋表面的15%,两极的环境正在迅速变化。提高对极地地区大气和海洋领域之间相互作用的认识是海洋表面-低层大气研究(SOLAS)项目的重点,这对于了解气候变化背景下的地球系统至关重要。然而,我们监测极地地区变化的速度和幅度以及评估其对全球其他地区影响的能力受到偏远和海冰覆盖的限制。海冰不仅支持生物活动和调节气体和气溶胶交换,而且还可能妨碍一些原位和遥感观测。虽然卫星遥感提供了海冰性质和范围的基线气候记录,但这些技术无法提供海冰内部和海冰以下的关键变量。最近机器人技术、建模和原位测量的进步为理解海洋-海洋冰-大气系统开辟了新的可能性,但仍然存在关键的知识空白。显然缺乏对所有变量和阶段的季节性和长期观测。海冰、海洋和大气领域的观测和模拟工作必须更好地联系起来,以实现对极地海洋和海冰环境的系统级理解。随着极地海洋变暖,海冰变得比以前更薄、更短暂,一系列物理化学和生物地球化学过程将发生巨大变化,如果还没有开始的话。海冰和海洋条件的这些变化将通过改变气溶胶、气溶胶前体、活性卤素和氧化剂的产生以及温室气体的交换来影响大气过程。量化哪些过程会因气候变化而增强或减弱,需要针对高纬度海洋环境制定量身定制的监测计划。利用正在进行的国际和多学科项目,如SOLAS牵头的努力,将海洋-海洋-冰-大气界面的研究联系起来,将最好地解决这个耦合系统中的未决问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Polar oceans and sea ice in a changing climate
Polar oceans and sea ice cover 15% of the Earth’s ocean surface, and the environment is changing rapidly at both poles. Improving knowledge on the interactions between the atmospheric and oceanic realms in the polar regions, a Surface Ocean–Lower Atmosphere Study (SOLAS) project key focus, is essential to understanding the Earth system in the context of climate change. However, our ability to monitor the pace and magnitude of changes in the polar regions and evaluate their impacts for the rest of the globe is limited by both remoteness and sea-ice coverage. Sea ice not only supports biological activity and mediates gas and aerosol exchange but can also hinder some in-situ and remote sensing observations. While satellite remote sensing provides the baseline climate record for sea-ice properties and extent, these techniques cannot provide key variables within and below sea ice. Recent robotics, modeling, and in-situ measurement advances have opened new possibilities for understanding the ocean–sea ice–atmosphere system, but critical knowledge gaps remain. Seasonal and long-term observations are clearly lacking across all variables and phases. Observational and modeling efforts across the sea-ice, ocean, and atmospheric domains must be better linked to achieve a system-level understanding of polar ocean and sea-ice environments. As polar oceans are warming and sea ice is becoming thinner and more ephemeral than before, dramatic changes over a suite of physicochemical and biogeochemical processes are expected, if not already underway. These changes in sea-ice and ocean conditions will affect atmospheric processes by modifying the production of aerosols, aerosol precursors, reactive halogens and oxidants, and the exchange of greenhouse gases. Quantifying which processes will be enhanced or reduced by climate change calls for tailored monitoring programs for high-latitude ocean environments. Open questions in this coupled system will be best resolved by leveraging ongoing international and multidisciplinary programs, such as efforts led by SOLAS, to link research across the ocean–sea ice–atmosphere interface.
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来源期刊
Elementa-Science of the Anthropocene
Elementa-Science of the Anthropocene Earth and Planetary Sciences-Atmospheric Science
CiteScore
6.90
自引率
5.10%
发文量
65
审稿时长
16 weeks
期刊介绍: A new open-access scientific journal, Elementa: Science of the Anthropocene publishes original research reporting on new knowledge of the Earth’s physical, chemical, and biological systems; interactions between human and natural systems; and steps that can be taken to mitigate and adapt to global change. Elementa reports on fundamental advancements in research organized initially into six knowledge domains, embracing the concept that basic knowledge can foster sustainable solutions for society. Elementa is published on an open-access, public-good basis—available freely and immediately to the world.
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