Surface Energy Balance on West Antarctica and the Ross Ice Shelf

西南极洲和罗斯冰架的表面能量平衡

基本信息

项目摘要

Atmospheric warming has been a major factor in the loss of ice shelves on the Antarctic Peninsula. In West Antarctica, oceanic warming is presently regarded as the largest source of stress on both the ice-shelves and at the grounding lines of the ice sheets. The loss of ice shelf buttressing and grounding line retreat may have already induced irreversible loss of Thwaites Glacier. To advance predictive models more data is needed regarding both water-induced fracturing on an ice shelf and marine ice cliff instability near the grounding line. This project will help advance understanding of atmospheric circulation and solar radiation over West Antarctica and the Ross Ice Shelf that lead to surface melting. In support of this project, and incorporating Antarctic science from this work, UCSD educators will sponsor a workshop series for exemplary middle and/or high school science teachers designed to address this need. Teacher participants will be carefully selected for their demonstrated leadership skills and will eventually become part of an cadre of "master" science teachers who will serve as local leaders in disseminating strategies and tools for addressing the NGSS (Ca Next Gen. of Sci. Eng. Stds.) to teachers throughout the county.For the summer field seasons requested, UCSD scientists will deploy a suite instruments to measure downwelling and net shortwave and longwave fluxes, sensible and latent heat fluxes, and near-surface meteorology. This suite of instruments will be self-reliant with power requirements and will be supportable in the field with a single Twin Otter aircraft. The investigators plan to deploy this suite as a remote ice camp with a field party of 2-3 personnel, making measurements for at up to one month during each of the sampled summer field seasons. These measurements will be analyzed and interpreted to determine mesoscale conditions that govern surface melt in West Antarctica, in the context of improving coupled climate model parameterizations.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.
大气变暖是南极半岛冰架消失的一个主要因素。在南极洲西部,海洋变暖目前被认为是冰架和冰原接地线的最大压力来源。冰架支撑的丧失和接地线的退缩可能已经导致了思韦茨冰川不可逆转的损失。为了改进预测模型,需要更多关于冰架上的水致压裂和接地线附近的海洋冰崖不稳定性的数据。该项目将有助于进一步了解导致南极西部和罗斯冰架表面融化的大气环流和太阳辐射。为了支持这个项目,并从这项工作中吸收南极科学,加州大学圣地亚哥分校的教育工作者将赞助一个系列研讨会,为模范的初中和/或高中科学教师设计,以满足这一需求。教师参与者将被精心挑选,因为他们展示了领导能力,最终将成为“大师”科学教师骨干的一部分,他们将作为当地的领导者,传播应对NGSS的战略和工具。Eng。向全县的教师分发。对于夏季野外季节的要求,加州大学圣地亚哥分校的科学家将部署一套仪器来测量下行和净短波和长波通量,感热通量和潜热通量,以及近地表气象学。这套仪器将在满足电力需求的情况下自给自足,并将在一架双水獭飞机上进行现场支持。研究人员计划将该套房部署为一个由2-3名野外人员组成的偏远冰营,在每个采样的夏季野外季节进行长达一个月的测量。在改进耦合气候模式参数化的背景下,将对这些测量结果进行分析和解释,以确定控制南极洲西部地表融化的中尺度条件。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。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Energetics of surface melt in West Antarctica
南极洲西部表面融化的能量
  • DOI:
    10.5194/tc-15-3459-2021
  • 发表时间:
    2021
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Ghiz, M L;Scott, R C;Vogelmann, A M;Lenaerts, J T;Lazzara, M;Lubin, D
  • 通讯作者:
    Lubin, D
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Dan Lubin其他文献

Aerosol‐Correlated Cloud Activation for Clean Conditions in the Tropical Atlantic Boundary Layer During LASIC
LASIC 期间热带大西洋边界层清洁条件的气溶胶相关云激活
  • DOI:
    10.1029/2023gl105798
  • 发表时间:
    2024
  • 期刊:
  • 影响因子:
    5.2
  • 作者:
    J. Dedrick;Lynn M. Russell;A. Sedlacek;C. Kuang;M. Zawadowicz;Dan Lubin
  • 通讯作者:
    Dan Lubin
Histologic characteristics and predictors of outcome in epithelial-myoepithelial carcinoma (EMC) of salivary gland: a multi-center study of 75 cases
  • DOI:
    10.1007/s00428-025-04159-6
  • 发表时间:
    2025-07-02
  • 期刊:
  • 影响因子:
    3.100
  • 作者:
    Bin Xu;Kartik Viswanathan;Michelle Afkhami;Mike Mikula;Dan Lubin;Kelly Magliocca;Dibisha Roy;Ronald Ghossein;Diana Bell;Lisa Rooper;Nora Katabi
  • 通讯作者:
    Nora Katabi

Dan Lubin的其他文献

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{{ truncateString('Dan Lubin', 18)}}的其他基金

Collaborative Research: Antarctic Low Cloud Interaction with Natural Aerosol (ALCINA)
合作研究:南极低云与天然气溶胶的相互作用(ALCINA)
  • 批准号:
    2130203
  • 财政年份:
    2023
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Standard Grant
Collaborative Research: First Scientific Priorities from the ARM West Antarctic Radiation Experiment
合作研究:ARM 西南极辐射实验的首要科学重点
  • 批准号:
    1443549
  • 财政年份:
    2015
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Standard Grant
Antarctic Cloud Physics: Fundamental Observations from Ross Island
南极云物理:罗斯岛的基本观测
  • 批准号:
    1141939
  • 财政年份:
    2012
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Standard Grant
ITR -- Polar Satellite Remote Sensing: Toward Full On-Line Access and Education
ITR——极地卫星遥感:迈向全面的在线访问和教育
  • 批准号:
    0218749
  • 财政年份:
    2002
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Standard Grant
The Arctic and Antarctic Research Center at the Scripps Institution of Oceanography
斯克里普斯海洋研究所北极和南极研究中心
  • 批准号:
    9806941
  • 财政年份:
    1999
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Continuing Grant
Antarctic Clouds and Climate
南极云层和气候
  • 批准号:
    9814151
  • 财政年份:
    1999
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Continuing Grant
Indian Ocean Experiment (INDOEX)
印度洋实验(INDOEX)
  • 批准号:
    9730276
  • 财政年份:
    1998
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Continuing Grant
Collaborative Research: Tethered Balloon Measurements of Cloud-Radiation-Sea Ice Interactions at the SHEBA Ice Camp: An Integrated Experimental and Modeling Study
合作研究:SHEBA 冰营的云-辐射-海冰相互作用的系留气球测量:综合实验和建模研究
  • 批准号:
    9701840
  • 财政年份:
    1997
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Continuing Grant
Contributions to SHEBA from Arctic Ocean Section 1994
1994 年北冰洋部分对 SHEBA 的贡献
  • 批准号:
    9504158
  • 财政年份:
    1995
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Standard Grant
The Arctic and Antarctic Research Center: A Unique Resource for Polar Science and Operations
北极和南极研究中心:极地科学和运营的独特资源
  • 批准号:
    9414276
  • 财政年份:
    1995
  • 资助金额:
    $ 48.96万
  • 项目类别:
    Continuing Grant

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度量测度空间上基于狄氏型和p-energy型的热核理论研究
  • 批准号:
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Constraining Yukon glacier surge dynamics using time series structure-from-motion analysis and surface energy balance modelling
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Collaborative Research: Assessing the Impact of Arctic Sea Ice Variability on the Greenland Ice Sheet Surface Mass and Energy Balance
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