Quantifying biological productivity and ocean carbon uptake in the NE Subarctic Pacific using observations and models
Quantifying biological productivity and ocean carbon uptake in the NE Subarctic Pacific using observations and models
批准号:
2241931
负责人:
Amanda Timmerman
金额:
$76.77万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2023
资助国家:
美国
项目状态:
未结题
起止时间:
2023-03-01 至 2026-02-28
中文摘要
地球系统模型是评估当前和未来地球环境变化的重要工具。然而,关于海洋吸收碳的模式,仍然存在许多模型分歧。该项目将进行实地观测和计算机模拟,以确定亚北极东北太平洋的生物碳吸收。该项目将把各种观测,如舰载、自主浮动、卫星测量等与高性能计算相结合。这个项目将有助于确定模型偏差的原因,并为未来的模型开发做出贡献。这项研究将从亚特兰大地区附近的HBCU聘请当地本科生作为学生助理,并通过夏季REU计划。该项目分为三个主题。首先是对生物生产力的体外、原位和卫星观测的整合。第二是开发区域碳和生态系统模型。第三,描述了生物生产力和海气碳通量的时空变异性。主要目标是通过结合现场和体外方法和建模来量化和减少区域生物碳吸收的不确定性。外地构成部分将在2024年6月利用P线时间序列巡航。将在五个主要站点进行孵化实验(13C、15NO3、15NH4)和正在进行的高分辨率O2/Ar测量。这将量化初级生产和碳出口。为了增加数据覆盖率,将纳入自主浮动和卫星观测。新的和现有的观测将用于验证和校准一个新的涡旋分辨率的三维区域生态系统和碳循环模型。该模型将被标定,然后将该模型用于进行多年代(1995-现在)的模拟。一系列敏感性模型实验将探索广泛的科学问题和假设,包括铁动力学、中尺度物理特征、气候模式和极端事件(如海洋热浪)的作用。这一奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
Earth system models are important tools to evaluate the current and future changes in the Earth’s environment. However, there are still many model disagreements about the patterns of carbon uptake by the oceans. This project will carry out field observations and computer modeling to determine the biological carbon uptake in the subarctic NE Pacific. This project will integrate various observations, for example, shipboard, autonomous float, satellite measurement, with high-performance computing. This project will help identify the causes of model biases and contribute to future model development. This study will engage local undergraduates as student assistants from nearby HBCUs in the Atlanta area and through summer REU program. The project is organized into three themes. First is the integration of in-vitro, in-situ and satellite observations of biological productivity. Second is the development of a regional carbon and ecosystem model. Third is characterization of spatial and temporal variability of biological productivity and air-sea carbon flux. The main objective is to quantify and reduce uncertainty in the regional biological carbon uptake through the combination of in situ and vitro methods and modeling. The field component will utilize the Line P time-series cruise in June 2024. Incubation experiments (13C, 15NO3, 15NH4) at five major stations will be conducted together with high-resolution underway O2/Ar measurements. This will quantify primary production and carbon export. To increase data coverage, autonomous floats and satellite observations will be incorporated. The new and existing observations will be used to validate and calibrate a new 3-dimensional regional ecosystem and carbon cycle model at eddy-resolving resolution. This model will be calibrated, then this model will be used to carry out multi-decadal simulation (1995-present). A suite of sensitivity model experiments will explore a wide range of scientific questions and hypotheses including the role of iron dynamics, mesoscale physical features, climate modes, and extreme events such as marine heat waves.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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