Collaborative Research: Unraveling North American Ice-Sheet Dynamics and Regional Sea-Level Change along the U.S. Mid-Atlantic over the Last Glacial Cycle

合作研究：揭示末次冰期期间北美冰盖动力学和美国大西洋中部沿线区域海平面变化

• 批准号: 2244722
• 负责人: Tamara Pico
• 金额: $ 26.68万
• 依托单位: University of California-Santa Cruz
• 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
• 起止时间: 2023-09-01 至 2026-08-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2244722&HistoricalAwards=false
• 关键词: Collaborative; Research; Unraveling; North; American

Rising sea levels impact coastal ecosystems and communities around the world. One of the most important factors influencing sea level rise locally is the vertical movement of the land surface. These adjustments can be caused by the growth and decay of glaciers and ice sheets which are often located thousands of kilometers away. A better understanding of this ice-land interaction—termed glacial isostatic adjustment—can improve predictions of future sea-level rise. This study will map and date shoreline deposits along the Eastern Shore of Virginia that were formed over the last ~120,000 years. The focus is on times when sea level was near to, or higher than present. These data will inform modeling of glacial isostatic adjustment and ice-sheet changes to better quantify the history of global ice sheet growth and decay. This research will address questions surrounding past regional sea-level and ice-sheet changes over the last glacial period. The work may also improve projections of the effect of glacial isostatic adjustment on regional sea-level rise into the future. Additionally, this project will support collaboration between the scientists and the non-profit Barrier Islands Center in Machipongo, Virginia. The collaboration will combine the geological results from the science team with local community knowledge of the region. This work will develop museum exhibits focused on the geology and physical history of the Virginia Eastern Shore. Global variations in ice volume through the last glacial cycle are a direct and sensitive measure of ice age climate change. However, regional (relative) sea level is controlled by a suite of local factors, primary among which is glacial isostatic adjustment. Significant uncertainty in the history of sea-level changes during the last glacial cycle—and the role of glacial isostatic adjustment in those—highlights the need for high-quality and well-dated sea-level markers across the ice-sheet growth phase (120,000 to 26,000 years ago). Mid-field sea-level observations (along the peripheral bulge of ice sheets) have the potential to bridge gaps in understanding between global sea level and local continental ice-sheet behavior, since relative sea level at these locations is sensitive to changes in the volume and extent in nearby ice sheets, as well as globally averaged sea-level changes. Focusing on the mid-field Eastern Shore of Virginia (USA), this study will first analyze high-resolution topographic and subsurface mapping data, assign indicative meanings to associated preserved Pleistocene coastal deposits, and develop a comprehensive geochronology to create a robust local, mid-field sea-level record over the period of growth of the last ice sheet. We will then perform state-of-the-art sea-level simulations using a range of possible ice-loading histories, which span the range of uncertainty on global mean sea level and ice-sheet geometries in order to gain insight into North American ice-sheet dynamics over this time period. In doing so, this study will better quantify the history of global ice sheet growth and decay and improve understanding of linkages between climate forcings and ice-sheet dynamics, with associated impacts on global eustatic, and mid-field relative sea level. Furthermore, this work will support the career development of 2 PhD students and an early-career PI, and mentor two undergraduate student research projects. The project will enable a collaboration with the non-profit Barrier Islands Center to engage the local community to share experiential knowledge to help create a museum exhibit.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.

海平面上升影响着世界各地的沿海生态系统和社区。影响局部海平面上升的最重要因素之一是陆地表面的垂直运动。这些调整可能是由冰川和冰盖的生长和衰退引起的，这些冰川和冰盖通常位于数千公里之外。更好地理解这种冰-陆相互作用-称为冰川均衡调整-可以改善对未来海平面上升的预测。本研究将绘制并测定弗吉尼亚州东海岸沿着海岸线沉积物的年代，这些沉积物是在过去~ 12万年间形成的。重点是海平面接近或高于现在的时期。这些数据将为冰川均衡调整和冰盖变化的建模提供信息，以更好地量化全球冰盖生长和衰退的历史。这项研究将解决围绕过去的区域海平面和冰盖变化在最后一个冰川时期的问题。这项工作还可能改善对未来冰川均衡调整对区域海平面上升影响的预测。此外，该项目将支持科学家与弗吉尼亚州Machipongo的非营利性屏障群岛中心之间的合作。这项合作将把科学小组的地质成果与当地社区对该地区的了解联合收割机结合起来。这项工作将开发以弗吉尼亚东海岸的地质和自然历史为重点的博物馆展览。在末次冰期循环中，全球冰量的变化是衡量冰期气候变化的一个直接而敏感的指标。然而，区域（相对）海平面是由一套当地的因素，其中主要是冰川均衡调整。末次冰期海平面变化历史的重大不确定性，以及冰川均衡调整在其中的作用，凸显了在冰盖生长阶段（120，000年至26，000年前）需要高质量和日期明确的海平面标志物。中场海平面观测（沿着冰盖的周边隆起）有可能弥合全球海平面和当地大陆冰盖行为之间的理解差距，因为这些位置的相对海平面对附近冰盖的体积和范围的变化以及全球平均海平面变化很敏感。本研究将重点放在弗吉尼亚州（美国）的中场东海岸，首先分析高分辨率地形和地下测绘数据，为相关的保存更新世海岸沉积物分配指示性意义，并开发一个全面的地质年代学，以创建一个强大的本地，中场海平面记录在最后一个冰盖的增长期间。然后，我们将使用一系列可能的冰加载历史进行最先进的海平面模拟，这些历史跨越全球平均海平面和冰盖几何形状的不确定性范围，以便深入了解这段时间内北美冰盖的动态。在这样做的过程中，这项研究将更好地量化全球冰盖生长和衰退的历史，并提高对气候强迫和冰盖动态之间的联系的理解，以及对全球海平面和中场相对海平面的相关影响。 此外，这项工作将支持2名博士生和一名早期职业PI的职业发展，并指导两名本科生的研究项目。该项目将与非营利机构Barrier Islands Center合作，让当地社区参与分享经验知识，以帮助创建博物馆展览。该奖项反映了NSF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。