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Towards a theory of the abyssal circulation

Towards a theory of the abyssal circulation
走向深海环流理论
批准号:
2149080
负责人:
Joern Callies
金额:
$32.67万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2022
资助国家:
美国
项目状态:
未结题
起止时间:
2022-02-01 至 2025-01-31

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中文摘要
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英文摘要
A revised picture is emerging of the deepest portion of the ocean's circulation. The mixing required to lighten dense bottom waters and that allows them to rise to mid-depth is strongly enhanced over rough topography. This project will work toward a dynamical theory that captures the interplay between the boundary transformations and interior flows and stratification. This work is important because the abyssal ocean has the capacity to store vast amounts of heat and carbon. A more complete understanding of what dynamical processes shape its circulation will help climate models capture its behavior and role in a changing climate. A pivotal role has been ascribed to the abyss in explaining the drawdown of atmospheric carbon dioxide during ice ages. Deeper insight into the dynamics of the abyssal circulation will also help understand better how it may have been different during these and other periods of Earth's history.The proposed work will build a hierarchy of dynamical models of the response of the abyssal circulation to bottom-intensified mixing on slopes with a focus on the two-way interaction between boundary layers on topographic slopes and the interior of the abyss. This interaction will be expressed explicitly using boundary layer theory. The approach will start with the local one-dimensional dynamics on slopes, then consider their coupling to the large-scale context in simple two-dimensional examples, and subsequently extend to idealized and increasingly realistic three-dimensional setups. This will connect recent work on bottom-intensified mixing on slopes to scaling theories for the abyssal overturning that are based on ocean basins with a flat bottom and vertical sidewalls. These dynamics will be explored using a planetary geostrophic model, whose reduced dynamics allow for direct dynamical insight and controlled numerical solutions that resolve all features, including the all-important boundary layers on topographic slopes.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.
期刊论文(1)
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会议论文
Coupling between Abyssal Boundary Layers and the Interior Ocean in the Absence of Along-Slope Variations
在没有沿坡变化的情况下深渊边界层与内海之间的耦合
DOI: 10.1175/jpo-d-22-0082.1
发表时间: 2023
期刊: Journal of Physical Oceanography
影响因子: 3.5
作者: [Peterson, Henry G., Callies, Jörn]
通讯作者: Callies, Jörn
Collaborative Research: Measuring abyssal warming with seismic Scholte waves
  • 批准号:
    2241664
  • 项目类别:
    Standard Grant
  • 资助金额:
    $9.59万
  • 财政年份:
    2023
  • 负责人:
    Joern Callies
  • 依托单位:
Seismic Ocean Thermometry
  • 批准号:
    2023161
  • 项目类别:
    Standard Grant
  • 资助金额:
    $61.15万
  • 财政年份:
    2020
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Understanding submesoscale tracer transport
  • 批准号:
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  • 项目类别:
    Standard Grant
  • 资助金额:
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  • 财政年份:
    2019
  • 负责人:
    Joern Callies
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