Role of radiative forcing on the sea ice melt-growth cycle in a changing Arctic marine environment - Northern**Research Supplement

不断变化的北极海洋环境中辐射强迫对海冰融化生长循环的作用 - Northern**Research Supplement

• 批准号: 444872-2013
• 负责人: Ehn, Jens
• 金额: $ 1.27万
• 依托单位: University of Manitoba
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Northern Research Supplement
• 财政年份: 2018
• 资助国家: 加拿大
• 起止时间: 2018-01-01 至 2019-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=649954
• 关键词: Role; radiative; forcing; sea; ice

The Arctic sea ice cover is in rapid decline due to global warming with yet another new record low reached in 2012. The diminishing ice cover is having a discernible impact on the polar marine environment. However, the extent of this impact on future changes to climate, carbon cycling and ecosystems remains uncertain. At the root is how surface radiative forcing affects changes in sea ice properties, and how these changes in turn modulate the forcing. Such interactions form the base of complex climate feedbacks operating in the Arctic. Considering the vastness of the area of sea ice (~10 million km2 or roughly the size of Canada) that forms and then melts each year, the importance of a comprehensive understanding of the processes driving this cycle cannot be overstated.** In this Northern Research Supplement proposal, I seek the additional funds required to support both field camp and ship-based sea ice research in the Canadian Arctic. The objective of the proposed research is to investigate how the melting of the sea ice is partitioned between surface, interior and bottom, and how much heat is retained in the upper ocean layers where it can delay fall freeze-up and slow ice growth. Our ability to predict future climate change and variability rests on understanding these processes. The focus is on radiative forcing and associated feedbacks as these interactions exert a dominant control on the surface energy balance in the Arctic. I will also utilize information from how radiation interacts with sea ice and seawater constituents to develop non-invasive optical methods to infer physical, biological and chemical properties in real-time at high spatial and temporal resolutions. ** The proposed research will advance our knowledge of sea ice processes and climate feedbacks, develop new optical techniques that addresses logistical challenges in data collection, train new students in Arctic environmental research and ultimately, benefit northerners by improving climate predictions that will help communities and various levels of government adapt to climate change.

由于全球变暖，北极海冰覆盖率迅速下降，2012年又有新的记录较低。冰覆盖量的减少是对极地海洋环境产生的明显影响。但是，这种影响对气候，碳循环和生态系统的未来变化的影响仍然不确定。根部是表面辐射强迫如何影响海冰特性的变化，以及这些变化如何调节强迫。这种相互作用构成了在北极运行的复杂气候反馈的基础。考虑到海冰地区的广阔（约1000万km2或大约是加拿大的大小），然后每年融化，对推动该周期的过程的全面了解的重要性不能被夸大。拟议的研究的目的是研究如何在表面，内部和底部划分海冰的熔化，以及在上海层中保留了多少热量，在那里它可以延迟降温并缓慢冰的生长。我们预测未来气候变化和可变性的能力取决于理解这些过程。重点是辐射强迫和相关的反馈，因为这些相互作用对北极的表面能量平衡产生了主要的控制。我还将利用从辐射与海冰和海水成分相互作用的信息来开发非侵入性光学方法，以在高空间和时间分辨率下实时推断物理，生物学和化学特性。 **拟议的研究将提高我们对海冰过程和气候反馈的了解，开发新的光学技术，以解决数据收集的后勤挑战，培训北极环境研究的新学生，并最终通过改善气候预测来使北方人受益，从而帮助北方人受益，这些预测将有助于社区和各种层次的政府政府适应气候变化。