Collaborative Proposal: Exploring Hypotheses of Southern Hemisphere Westerly Wind Changes on Southern Ocean Circulation and Biogeochemistry

合作提案：探索南半球西风变化对南大洋环流和生物地球化学的假设

• 批准号: 1537496
• 负责人: John Chiang
• 金额: $ 3.3万
• 依托单位: University of California-Berkeley
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2015
• 资助国家: 美国
• 起止时间: 2015-10-01 至 2018-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1537496&HistoricalAwards=false
• 关键词: Collaborative; Proposal; Exploring; Hypotheses; Southern

The circulation of the Southern Ocean plays a prominent role in regulating Earth's climate, in particular connecting the deep ocean to the surface. This connection holds particular importance for the Earth's carbon cycle as upwelling of waters from the deep ocean brings stored carbon of the deep to the surface, eventually entering into the atmosphere as carbon dioxide. Increased upwelling is thought to have brought about the initial rise in atmospheric CO2 concentrations during the last deglaciation, caused by changes to the surface westerlies and resulting changes to the wind-driven upwelling. This project investigates a recent hypothesis for how the westerlies changed during this time period affects Southern ocean circulation and carbon cycle, through the use of a state-of-the-art climate model. The predictions of this hypothesis will be contrasted against those made by the "annular-mode" view for westerly changes that dominates current thinking, and both compared against available paleoproxy observations. The research provides concrete tests
to each hypothesis, and the process will help advance our understanding of how southern hemisphere westerlies affect the ocean climate and carbon cycle. The project will also enhance collaboration between two US-based scientists with an overseas collaborator based in Taiwan.Previous studies have largely assumed that paleo-westerly changes were zonally uniform, analogous to the so-called "annular mode" behavior that dominates year-to-year variations in the southern hemisphere westerlies today. However, in reality there are insufficient paleoproxy data to confirm this interpretation, and in a recent study one of the PIs proposed an alternative hypothesis for westerly changes through the modulation of the South Pacific Split Jet. The Split Jet is a regional feature of the South Pacific whereby the core of the westerlies split into two around Australia, and this split extends across the Pacific. Based on dynamical reasoning and comparison to paleoproxy records, the PI argued that the Split Jet feature weakened during Heinrich events, in particular Heinrich event 1 that preceded the last deglaciation. In this study, the consequences for a weaker Split Jet on the Southern ocean circulation and biogeochemistry will be investigated through idealized simulations using the ocean component of the Community Earth System Model version 1 with a simple ocean biogeochemistry module. Focus will be placed on understanding changes to the ocean surface temperature and frontal locations, changes to the upwelling and carbon fluxes. These simulations will be compared and contrasted against simulations where annular-mode like westerly changes is imposed. Through comparison between these simulations with available ocean paleoproxies, an assessment can be made as to which westerly configuration was more likely. If the Split Jet hypothesis turns out to be more correct, it has strong implications for our conceptualization and understanding of Southern ocean climate and circulation changes.

南大洋的环流在调节地球气候方面发挥着重要作用，特别是将深海与地表连接起来。 这种联系对于地球的碳循环特别重要，因为深海海水的上涌将深海储存的碳带到地表，最终以二氧化碳的形式进入大气层。 人们认为，上一次冰消期期间上升流的增加导致了大气二氧化碳浓度的最初上升，这是由地表西风带的变化以及风驱动的上升流的变化引起的。 该项目通过使用最先进的气候模型，研究了关于这一时期西风带变化如何影响南大洋环流和碳循环的最新假设。 这一假设的预测将与主导当前思维的西风变化的“环形模式”观点所做出的预测进行对比，并且两者都与现有的古代理观测结果进行比较。 该研究为每个假设提供了具体的测试，该过程将有助于加深我们对南半球西风带如何影响海洋气候和碳循环的理解。 该项目还将加强两名美国科学家与一名台湾海外合作者之间的合作。之前的研究很大程度上假设古西风变化是地带性均匀的，类似于每年主导的所谓“环形模式”行为。今天南半球西风带的年变化。 然而，实际上没有足够的古替代数据来证实这一解释，在最近的一项研究中，一位 PI 提出了通过南太平洋分裂急流的调制来解释西风变化的替代假设。 分裂急流是南太平洋的一个区域特征，西风带的核心在澳大利亚周围分裂成两部分，并且这种分裂延伸到整个太平洋。 基于动力学推理和与古代理记录的比较，PI 认为分裂急流特征在海因里希事件期间减弱，特别是在最后一次冰消之前的海因里希事件 1。 在这项研究中，将使用社区地球系统模型版本 1 的海洋组件和简单的海洋生物地球化学模块，通过理想化模拟来研究较弱的分裂急流对南部海洋环流和生物地球化学的影响。 重点将放在了解海洋表面温度和锋面位置的变化、上升流和碳通量的变化。 这些模拟将与施加类似西风变化的环形模式的模拟进行比较和对比。 通过将这些模拟与可用的海洋古代理进行比较，可以评估哪种西风配置更有可能。 如果分裂射流假说被证明更为正确，它将对我们对南大洋气候和环流变化的概念化和理解产生重大影响。