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Collaborative Research: IPY: Dynamic Controls on Tidewater Glacier Retreat

Collaborative Research: IPY: Dynamic Controls on Tidewater Glacier Retreat
合作研究:IPY:潮水冰川退缩的动态控制
批准号:
0732726
负责人:
W. Tad Pfeffer
金额:
$61.54万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2008
资助国家:
美国
项目状态:
已结题
起止时间:
2008-04-15 至 2011-03-31

项目摘要

项目成果

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中文摘要
翻译
智力上的优点。主要研究人员将研究阿拉克萨中南部快速退缩的哥伦比亚冰川的动态变化。像哥伦比亚冰川这样的潮汐冰川(TWG)终止于海洋,值得特别关注,因为它们表现出全球所有冰川中最大的和强烈的非线性动态体积变化。此外,大多数冰盖的质量损失发生在海洋结束出口冰川,显示动态不稳定性非常相似的TWG。然而,这些冰川对气候强迫的反应仍然知之甚少。他们将继续对哥伦比亚冰川进行长达30年的观测,并研究它与迅速退缩的格陵兰出口冰川之间的相似之处。项目目标旨在提高对未来TWG体积变化的预测能力,这是全球海平面上升的主要组成部分。各种测量,包括垂直航空摄影测量(和随后的功能跟踪),地面延时摄影测量,机载雷达,GPS测量和气象监测将提供强大的约束,为逆和正演模拟的应力和流场。 人们普遍认识到需要更好地了解气候强迫、冰川动力学和冰量变化之间的相互作用,并在IPCC 2007年决策者摘要、IPCC实施计划、IPY欧盟和国际冰川年中提出了更好地观测冰川的建议。GLACIODYN倡议和NSF呼吁建立北极观测网络。《冰川学实施计划》和《冰川学动态》都将哥伦比亚冰川特别列为一个关键的冰川学遗址。这项研究与GLACIODYN的目标高度一致,并得到了指导委员会的认可。更广泛的影响。由于其数量庞大,小型冰川仍然主导着冰冻圈对全球海平面上升的贡献。这一贡献的最大不确定性来自TWG,其中体积变化由未测量和知之甚少的动态过程控制。冰川和冰盖的快速淡水输入直接影响洋流,灾难性的退缩影响了全球气候,海因里希事件就是明证。TWG快速体积变化的区域和局部变化影响峡湾的几何形状和环流,同时暴露新的陆地,这导致陆地生态系统的巨大变化,包括一些最强的观测到的均衡反弹信号。这项研究将通过与欧洲同事合作,建立新的伙伴关系,对推进地面摄影测量方法感兴趣,并通过与A。维利这项活动是来自科罗拉多大学和华盛顿大学的研究人员之间的合作,有很强的教育成分,涉及本科生和两名研究生。外联将通过INSTAAR和国家冰雪数据中心(NSIDC)提供的渠道进行,主要研究者在阿拉斯加巴尔德斯和华盛顿大学开展的当地外联活动。将向GLACIODYN外联协调员提供数据,协调员将使用虚拟地球仪技术进行项目可视化。研究结果将发表在同行评审的期刊上,在国家和国际会议上发表演讲,以及举办以软件和算法开发为重点的小型讲习班,并将在国家统计数据中心和联合国志愿人员组织存档。
英文摘要
Intellectual merit. The Principal Investigators will study both ongoing and historical changes in dynamics at the rapidly retreating Columbia Glacier, in south central Alaksa. Tidewater glaciers (TWGs) like Columbia Glacier terminate in the ocean and merit special attention because they exhibit some of the largest and strongly non-linear dynamic volume changes of all glaciers worldwide. In addition, most ice sheet mass loss occurs at marine-ending outlet glaciers that display dynamic instabilities very similar to TWG. Yet, the response of these glaciers to climate forcing remains very poorly understood. They will continue an unmatched 30-year record of observations at Columbia Glacier and to study the similarities between it and the rapidly retreating Greenland outlet glaciers. Project goals are aimed at a predictive capability for future TWG volume changes, which are a dominant constituent of global sea level rise. A variety of measurements including vertical aerial photogrammetry (and subsequent feature-tracking), terrestrial time-lapse photogrammetry, airborne radar, GPS surveying, and meteorological monitoring will provide robust constraints for both inverse and forward modeling of the stress and flow fields. The need for a better understanding of the interaction between climate forcing, glacier dynamics and ice volume change is widely recognized and has led to recommendations for better glacier observations in the the IPCC 2007 Summary for Policymakers, the SEARCH Implementation Plan, the IPY E.U. initiative GLACIODYN, and the NSF call for an Arctic Observing Network. Both the SEARCH Implementation Plan and GLACIODYN list Columbia Glacier specifically as a key glaciological site. This study strongly aligned with the goals of GLACIODYN, and has been endorsed by the steering committee. Broader impacts. Because of their large numbers, small glaciers still dominate the cryosphere's contribution to global sea level rise. The largest uncertainties in this contribution are from TWG where volume changes are controlled by unmeasured and poorly understood dynamical processes. Rapid freshwater inputs of glaciers and ice sheets directly affect ocean currents, and catastrophic retreats have affected global climate, as evidenced through Heinrich Events. Regional and local changes from rapid volume change at TWGs affect fjord geometry and circulation while exposing new landmass, which causes large changes in terrestrial ecosystems including some of the strongest observed isostatic rebound signals. This study will create new partnerships through collaborations with European colleagues interested in advancing terrestrial photogrammetric methodology, and through a forward modeling collaboration with A. Vieli. The activity is a collaboration between researchers from the Universities of Colorado and Washington, and has a strong educational component, involving undergraduates, and two graduate students. Outreach will occur through channels offered by INSTAAR and National Snow and Ice Data Center (NSIDC), local outreach activities conducted by the Principal Investigators in Valdez, Alaska and University of Washington. Data will be provided to the GLACIODYN outreach coordinator, who will use Virtual Globe technology for project visualization. Results will appear in peer reviewed journals, presentations at national and international meetings, and small workshops focusing on software and algorithm development, and will be archived at NSIDC and UNAVCO
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Collaborative Research: Greenland Ice Sheet Basal Hydrology and Sliding Dynamics - The Proof of the Drill
  • 批准号:
    0909503
  • 项目类别:
    Standard Grant
  • 资助金额:
    $10.0万
  • 财政年份:
    2009
  • 负责人:
    W. Tad Pfeffer
  • 依托单位:
Outreach and Educational Support for Ongoing Research at Columbia Glacier, Alaska
  • 批准号:
    0741610
  • 项目类别:
    Standard Grant
  • 资助金额:
    $7.5万
  • 财政年份:
    2008
  • 负责人:
    W. Tad Pfeffer
  • 依托单位:
SGER: Photogrammetric/Media Camera Support for Alaska Glacier Observations
  • 批准号:
    0731541
  • 项目类别:
    Standard Grant
  • 资助金额:
    $0.0万
  • 财政年份:
    2007
  • 负责人:
    W. Tad Pfeffer
  • 依托单位:
Support for Graduate Students in the Annual Arctic Workshop
  • 批准号:
    0713864
  • 项目类别:
    Standard Grant
  • 资助金额:
    $16.37万
  • 财政年份:
    2007
  • 负责人:
    W. Tad Pfeffer
  • 依托单位:
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)