OCE-PRF: Quantifying the Chukchi Sea's role in modulating present and future changes of Pacific waters in the Arctic

OCE-PRF：量化楚科奇海在调节北极太平洋水域当前和未来变化中的作用

• 批准号: 2126646
• 负责人: Marion Alberty
• 金额: $ 33.55万
• 依托单位: Princeton University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-12-01 至 2024-11-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2126646&HistoricalAwards=false
• 关键词: OCE; PRF; Quantifying; Chukchi; Sea

This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2).The Arctic is changing quickly as the ocean and atmosphere warm and sea ice shrinks. These changes impact the global climate, regional ecosystems, native communities, and geopolitical and economic decision-making. The sea ice loss has been greatest in the seas off the coast of Alaska, the Chukchi and Beaufort Seas. The majority of this loss is due to warming oceans in the region. Future sea ice loss will depend on how the Chukchi and Beaufort Seas gain heat. This work aims to create a detailed accounting of how heat moves through the Chukchi Sea from the Pacific Ocean before either being released to the atmosphere or entering into the Beaufort Sea. This work will use state-of-the-art climate models from the National Oceanic and Atmospheric Administration (NOAA) Geophysical Fluid Dynamics Laboratory (GFDL) to investigate both the current and future pathways of heat through this region. The scientific impact of this work is to provide important insights into how the Chukchi and Beaufort Seas have gained and will continue to gain heat. In addition, this work will also help improve future predictions of Arctic sea ice and ecosystem conditions, providing important information to the public, policy makers and industry. The Chukchi Sea is a key marginal sea in the Arctic where warming Pacific Waters are modified through surface fluxes before subducting below the Beaufort Gyre halocline. While a critically important region for understanding current climate and predicting future changes, it's exact role in modulating Pacific Water heat remains unclear. The scientific goals of this proposal are to determine the fate of Pacific Water heat using a closed heat budget of the Chukchi Sea, identify the physical processes that set the balance between heat budget terms and their time scales of variability, and quantify the role of sea ice in the Chukchi Sea's heat budget. The National Oceanic and Atmospheric Administration (NOAA) Geophysical Fluid Dynamics Laboratory (GFDL) coupled climate model, CM4.0, will be used to produce closed mean annual and seasonal heat budgets of the Chukchi Sea. These mean heat budgets will provide a framework for understanding the temporal variability of individual heat budget terms in past and future simulations and guide investigation into the physical processes responsible for modulating terms on a range of time scales, including the influence of Marine Heat Waves on ocean heat transport through the Bering Strait. Through analysis of CM4.0’s sea ice model, I propose to determine the role of sea ice extent and advection on the surface flux component of the Chukchi Sea heat budget. The scientific impact of this work is to provide important insights into how the Chukchi and Beaufort Seas have gained and will continue to gain heat. In addition, this work will also help improve future predictions of Arctic sea ice and ecosystem conditions, providing important information to the public, policy makers and industry.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.

该奖项全部或部分由《2021年美国救援计划法案》（公法117-2）资助。随着海洋和大气变暖以及海冰缩小，北极正在迅速变化。这些变化影响着全球气候、区域生态系统、土著社区以及地缘政治和经济决策。阿拉斯加海岸、楚科奇海和波弗特海的海冰损失最为严重。这种损失的主要原因是该地区海洋变暖。未来的海冰损失将取决于楚科奇海和波弗特海如何获得热量。这项工作的目的是详细描述热量如何从太平洋穿过楚科奇海，然后释放到大气中或进入波弗特海。这项工作将使用来自美国国家海洋和大气管理局（NOAA）地球物理流体动力学实验室（GFDL）的最先进的气候模型来研究该地区当前和未来的热量路径。这项工作的科学影响是为楚科奇海和波弗特海如何获得并将继续获得热量提供了重要的见解。此外，这项工作还将有助于改善对北极海冰和生态系统状况的未来预测，为公众、政策制定者和工业界提供重要信息。楚科奇海是北极的一个关键边缘海，在这里，变暖的太平洋海水通过表面通量被改变，然后俯冲到波弗特环流盐斜之下。虽然它是了解当前气候和预测未来变化的一个至关重要的区域，但它在调节太平洋水温方面的确切作用尚不清楚。本提案的科学目标是利用楚科奇海的封闭热收支来确定太平洋水热的命运，确定在热收支项及其变率时间尺度之间设定平衡的物理过程，并量化海冰在楚科奇海热收支中的作用。美国国家海洋和大气管理局（NOAA）地球物理流体动力学实验室（GFDL）耦合气候模式CM4.0将用于生成楚科奇海的闭合平均年和季节热量收支。这些平均热收支将为理解过去和未来模拟中单个热收支项的时间变化提供一个框架，并指导研究在一系列时间尺度上负责调节项的物理过程，包括海洋热浪对通过白令海峡的海洋热输送的影响。通过对CM4.0海冰模式的分析，提出确定海冰范围和平流对楚科奇海热收支表面通量分量的作用。这项工作的科学影响是为楚科奇海和波弗特海如何获得并将继续获得热量提供了重要的见解。此外，这项工作还将有助于改善对北极海冰和生态系统状况的未来预测，为公众、政策制定者和工业界提供重要信息。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。