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Collaborative Research: Formation and Persistence of Benthic Biological Hotspots in the Pacific Arctic

Collaborative Research: Formation and Persistence of Benthic Biological Hotspots in the Pacific Arctic
合作研究:北极太平洋底栖生物热点的形成和持续
批准号:
1604047
负责人:
Rubao Ji
金额:
$55.47万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2016
资助国家:
美国
项目状态:
已结题
起止时间:
2016-08-01 至 2021-07-31

项目摘要

项目成果

Rubao Ji的其他基金

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中文摘要
翻译
在北白令海和楚科奇海的四个主要底栖生物热点地区,观察到大型底栖动物生物量持续较高。这些高生产力的底栖生物群落具有重要的生态意义,为底栖食性海洋哺乳动物和海鸟提供了丰富的猎物。这笔赠款支持探索促成这些海底热点形成的物理和生物过程,并确定北极系统的变化(包括冰、海洋和大气强迫)将如何影响它们的形成和持续。更好地了解这些海底热点的形成和持续机制很重要,需要在本研究中采取大气-冰-海洋系统办法,因为这些形成机制涉及北极系统的多个组成部分,包括海冰和海洋过程的生物和物理组成部分以及大气强迫。该小组将整合一套模型,包括冰-海洋-生态系统耦合模型和拉格朗日粒子跟踪模型,以评估有机质的来源、运输途径和对海底群落的供应。模拟将跨越整个系统,从大气强迫向下到粒子输出通量。为了从机制上了解北极太平洋区域的生态系统结构,需要对底-上层耦合进行明确建模,并将提供基线信息,以便更好地预测未来生态系统的变化。一旦模型验证和综合观测完成,该项目将广泛描述整个白令海和楚科奇海北部海底热点的现有和潜在位置和碳源,包括目前采样不足的区域,以及它们对持续气候和环境变化的脆弱性。它还将更好地了解促成海底热点形成的机制(例如,浮游动物捕食、平流生产和/或营养输入的季节和年际变化、洋流、汇合、湍流和颗粒聚集在热点形成中的作用、海冰形成的时间、覆盖和撤退、大气强迫的年际或长期差异)。两者都有助于未来实地工作的设计,因为热点位置的全面空间分布可以指导以地点为基础的实地工作,而模拟的生态系统过程和转变的相对重要性将有助于过程研究和分配研究的需要。随着持续的气候变化,大气强迫和洋流可能会在强度和方向上发生变化,可能会改变这些机制的汇聚促进碳出口和海底热点形成的地点。了解这些相互关联的机制如何运作以产生现有的海底热点,将使我们能够经验地预测它们未来的持久性或重新定位。建模工作的结果既可被科学界用于指导未来的实地工作和建模工作,也可更广泛地被管理人员和政策制定者用于指导管理和商业战略和准则的制定和执行。这项工作将包括主要侧重于K-12教育的外联活动,重点是大气强迫、海冰、洋流和海底-中上层海洋耦合对白令海/楚科奇海系统的重要性,以及持续气候变化对该系统的影响。
英文摘要
Persistently high macrofaunal benthic biomass has been observed at four major benthic hotspots in the Northern Bering and Chukchi Seas. These highly productive benthic communities are ecologically important and provide abundant prey for benthic-feeding marine mammals and seabirds. This grant supports the exploration of the physical and biological processes that contribute to the formation of these benthic hotspots, and a determination of how changes in the Arctic system (including ice, ocean, and atmospheric forcing) will affect their formation and persistence. A better understanding of the mechanisms for the formation and persistence of these benthic hotspots is important and requires the atmosphere-ice-ocean system approach taken in this study, since these formation mechanisms involve multiple components of the Arctic system, including both biological and physical components of sea ice and ocean processes and atmospheric forcing. The group will integrate a suite of models, including an ice-ocean-ecosystem coupled model and a Lagrangian particle-tracking model, to evaluate source, transport pathway, and supply of organic matter to the benthic community. The modeling will span the entire system from atmospheric forcing down to particle export flux. Explicitly modeling benthic-pelagic coupling is needed for a mechanistic understanding of the ecosystem structure in the Pacific Arctic region and will provide baseline information to better predict future ecosystem shifts. Once the model validation and synthesis with observations are accomplished, the project will have a broad-scale description of the existing and potential locations of benthic hotspots and carbon sources for benthic hotspots across the entire northern Bering and Chukchi Seas, including regions that are presently under-sampled, and their vulnerabilities to ongoing climate and environmental changes. It will also have a better understanding of the mechanisms contributing to benthic hotspot formation (e.g., zooplankton grazing, seasonal and inter-annual variability in advected inputs of production and/or nutrients, role of currents, convergences, turbulence, and particle aggregation in hotspot formation, timing of sea ice formation, cover, and retreat, inter-annual or long-term differences in atmospheric forcing). Both can contribute to the design of future field efforts, since the comprehensive spatial distribution of hotspot location can guide place-based field efforts and the relative importance of modeled ecosystem processes and transformations will inform needs for process studies and distributional studies. With ongoing climate change, atmospheric forcing and ocean currents are likely to change in strength and direction, potentially modifying the locations where the convergence of these mechanisms promotes enhanced carbon export and benthic hotspot formation. Understanding of how these linked mechanisms operate to produce the existing benthic hotspots will permit us to predict empirically their future persistence or relocation. The results of the modeling effort can be used both by the scientific community in guiding future fieldwork and modeling efforts and more broadly by managers and policy makers in guiding the development and implementation of management and commercial strategies and guidelines. This work will include outreach activities primarily focused on K-12 education, focusing on the importance of atmospheric forcing, sea ice, currents, and benthic-pelagic coupling to the Bering/Chukchi Sea system and the impacts of ongoing climate change on that system.
期刊论文(0)
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会议论文
Collaborative Research: Mechanisms supporting persistence of a key plankton species during climate change on the Northwest Atlantic continental shelf
Collaborative Research: Phytoplankton Phenology in the Antarctic: Drivers, Patterns, and Implications for the Adelie Penguin
Collaborative Research: Changes in Arctic Sea Ice and their Impact on Timing of Life History and Production of Zooplankton
Marine Metapopulation Connectivity: Modeling, Estimation and Demographic Consequences
国内基金
海外基金
Research on Quantum Field Theory without a Lagrangian Description
  • 批准号:
    24ZR1403900
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    SATOSHI NAWATA
  • 依托单位:
Cell Research
Cell Research
Cell Research (细胞研究)