Collaborative Research: Closing the Gaps in Climate Models' Surface Albedo Schemes of Processes Driving the Darkening of the Greenland Ice Sheet

合作研究:缩小气候模型表面反照率方案中导致格陵兰冰盖变暗的过程的差距

基本信息

  • 批准号:
    1713072
  • 负责人:
  • 金额:
    $ 40.52万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    2017
  • 资助国家:
    美国
  • 起止时间:
    2017-09-15 至 2023-02-28
  • 项目状态:
    已结题

项目摘要

Surface albedo is a measure of the percentage of solar radiation that is reflected by a medium. The higher (lower) the albedo, the lower (higher) is the amount of solar energy absorbed by the medium. Albedo plays a critical role on the Greenland Ice Sheet, where absorbed solar radiation is the dominant driver of surface melt during summer. The evolution of albedo on the Greenland Ice Sheet is primarily driven by changes in snow grain size, the presence of liquid water on the surface, the exposure of bare ice, and the presence of light-absorbing impurities in the snow and ice. Such impurities include soot, dust, and biological constituents like bacteria and algae. Interactions between biological impurities and snow physical processes (e.g., metamorphism and melt redistribution) are important because they can drive positive feedbacks in which total melt is amplified. Despite their importance, these processes relating biological constituents to snow and ice evolution are currently either absent or poorly represented in models used to simulate current estimates and future projections of the contribution of Greenland to sea level rise. Through an interdisciplinary and collaborative effort, this project will integrate state of the art knowledge of how biological activity impacts albedo into climate models. This will help reduce uncertainties of the contribution of Greenland to sea level rise and will also improve our understanding of interactions between the ice sheet and the atmosphere.The regional climate and Earth System models that will be applied in our study are open-source models, such as e.g., the Community Earth System Model). Model improvements that are implemented will be released for use by other researchers in a timely way. The project includes the involvement of a postdoctoral fellow, and hence training of young investigators to address complex and yet crucial science questions through an interdisciplinary effort. Results from this project will be communicated to the media and public, thereby promoting deeper knowledge of the processes affecting the surface mass balance of the Greenland Ice Sheet.
地表反照率是测量太阳辐射被介质反射的百分比。反照率越高(越低),介质吸收的太阳能量越低(越高)。反照率在格陵兰冰盖上起着至关重要的作用,在那里,吸收的太阳辐射是夏季地表融化的主要驱动力。格陵兰冰盖反照率的演变主要是由雪颗粒大小的变化、表面液态水的存在、裸露冰的暴露以及冰雪中吸收光的杂质的存在所驱动的。这些杂质包括烟灰、灰尘和细菌、藻类等生物成分。生物杂质与雪物理过程(如变质作用和熔体再分配)之间的相互作用是重要的,因为它们可以驱动正反馈,其中总熔体被放大。尽管这些过程很重要,但在用于模拟格陵兰对海平面上升贡献的当前估计和未来预测的模式中,这些与冰雪演变有关的生物成分的过程目前要么不存在,要么代表性不足。通过跨学科和协作的努力,该项目将把生物活动如何影响反照率的最新知识整合到气候模型中。这将有助于减少格陵兰对海平面上升贡献的不确定性,也将提高我们对冰盖与大气之间相互作用的理解。我们研究中应用的区域气候和地球系统模型是开源模型,例如社区地球系统模型(Community Earth System Model)。已经实现的模型改进将及时发布,供其他研究人员使用。该项目包括一名博士后的参与,从而培训年轻的研究人员通过跨学科的努力来解决复杂而关键的科学问题。该项目的结果将向媒体和公众传播,从而促进对影响格陵兰冰盖表面物质平衡的过程的更深入了解。

项目成果

期刊论文数量(5)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Assessing bare-ice albedo simulated by MAR over the Greenland ice sheet (2000–2021) and implications for meltwater production estimates
  • DOI:
    10.5194/tc-16-4185-2022
  • 发表时间:
    2022-10
  • 期刊:
  • 影响因子:
    0
  • 作者:
    R. Antwerpen;M. Tedesco;X. Fettweis;P. Alexander;W. J. van de Berg
  • 通讯作者:
    R. Antwerpen;M. Tedesco;X. Fettweis;P. Alexander;W. J. van de Berg
Simulated Greenland Surface Mass Balance in the GISS ModelE2 GCM: Role of the Ice Sheet Surface
GISS ModelE2 GCM 中模拟的格陵兰表面质量平衡:冰盖表面的作用
  • DOI:
    10.1029/2018jf004772
  • 发表时间:
    2019
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Alexander, P. M.;LeGrande, A. N.;Fischer, E.;Tedesco, M.;Fettweis, X.;Kelley, M.;Nowicki, S. M. J.;Schmidt, G. A.
  • 通讯作者:
    Schmidt, G. A.
How fast is the Greenland ice sheet melting?
格陵兰冰盖融化的速度有多快?
  • DOI:
    10.1080/15230430.2021.1946241
  • 发表时间:
    2021
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Scambos, Ted;Straneo, Fiamma;Tedesco, Marco
  • 通讯作者:
    Tedesco, Marco
Mapping Ice Algal Blooms in Southwest Greenland From Space
  • DOI:
    10.1029/2018gl080455
  • 发表时间:
    2018-11
  • 期刊:
  • 影响因子:
    5.2
  • 作者:
    Shujie Wang;M. Tedesco;Min Xu;P. Alexander
  • 通讯作者:
    Shujie Wang;M. Tedesco;Min Xu;P. Alexander
Spectral attenuation coefficients from measurements of light transmission in bare ice on the Greenland Ice Sheet
  • DOI:
    10.5194/tc-15-1931-2021
  • 发表时间:
    2021-04
  • 期刊:
  • 影响因子:
    0
  • 作者:
    M. Cooper;L. Smith;Å. Rennermalm;M. Tedesco;R. Muthyala;S. Leidman;S. Moustafa;J. Fayne
  • 通讯作者:
    M. Cooper;L. Smith;Å. Rennermalm;M. Tedesco;R. Muthyala;S. Leidman;S. Moustafa;J. Fayne
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Marco Tedesco其他文献

Concurrent superimposed ice formation and meltwater runoff on Greenland’s ice slabs
格陵兰冰原上的并发叠加冰层形成和融水径流
  • DOI:
    10.1038/s41467-025-59237-9
  • 发表时间:
    2025-05-14
  • 期刊:
  • 影响因子:
    15.700
  • 作者:
    Andrew Tedstone;Horst Machguth;Nicole Clerx;Nicolas Jullien;Hannah Picton;Julien Ducrey;Dirk van As;Paolo Colosio;Marco Tedesco;Stef Lhermitte
  • 通讯作者:
    Stef Lhermitte
Comparative analysis of morphological, mineralogical and spectral properties of cryoconite in Jakobshavn Isbræ, Greenland, and Canada Glacier, Antarctica
格陵兰岛雅各布港伊斯布雷和南极洲加拿大冰川的冰石形态、矿物学和光谱特性的比较分析
  • DOI:
  • 发表时间:
    2013
  • 期刊:
  • 影响因子:
    2.9
  • 作者:
    Marco Tedesco;Christine M. Foreman;J. Anton;N. Steiner;T. Schwartzman
  • 通讯作者:
    T. Schwartzman
A new surface meltwater routing model for use on the Greenland Ice Sheet surface
用于格陵兰冰盖表面的新表面融水路径模型
  • DOI:
    10.5194/tc-12-3791-2
  • 发表时间:
    2018-11
  • 期刊:
  • 影响因子:
    0
  • 作者:
    Kang Yang;Laurence C. Smith;Leif Karlstrom;Matthew G. Cooper;Marco Tedesco;Dirk van As;Xiao Cheng;Zhuoqi Chen;Manchun Li
  • 通讯作者:
    Manchun Li

Marco Tedesco的其他文献

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{{ truncateString('Marco Tedesco', 18)}}的其他基金

EAGER: Quantifying Spatial Distribution of Micro- and Nanoplastics along an Antarctic Traverse
EAGER:量化沿南极横贯线的微米和纳米塑料的空间分布
  • 批准号:
    2334490
  • 财政年份:
    2023
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Collaborative Research: EAGER: Generation of High Resolution Surface Melting Maps over Antarctica using Regional Climate Models, Remote Sensing and Machine Learning
合作研究:EAGER:利用区域气候模型、遥感和机器学习生成南极洲高分辨率表面融化地图
  • 批准号:
    2136938
  • 财政年份:
    2022
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
EAGER: spatio-temporal variability of microplastics in ocean and river cores using fluorescence microscopy
EAGER:使用荧光显微镜观察海洋和河流核心中微塑料的时空变化
  • 批准号:
    2019835
  • 财政年份:
    2020
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Collaborative Research: Linking sea ice and snow cover changes to Greenland mass balance through stratospheric and tropospheric pathways
合作研究:通过平流层和对流层路径将海冰和积雪变化与格陵兰岛质量平衡联系起来
  • 批准号:
    1901603
  • 财政年份:
    2019
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Collaborative Research: Assessing the Impact of Arctic Sea Ice Variability on the Greenland Ice Sheet Surface Mass and Energy Balance
合作研究:评估北极海冰变化对格陵兰冰盖表面质量和能量平衡的影响
  • 批准号:
    1643187
  • 财政年份:
    2016
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Collaborative Research: Refreezing in the firn of the Greenland ice sheet: Spatiotemporal variability and implications for ice sheet mass balance
合作研究:格陵兰冰盖冰层的重新冻结:时空变化及其对冰盖质量平衡的影响
  • 批准号:
    1603331
  • 财政年份:
    2016
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Collaborative Research: Assessing the Impact of Arctic Sea Ice Variability on the Greenland Ice Sheet Surface Mass and Energy Balance
合作研究:评估北极海冰变化对格陵兰冰盖表面质量和能量平衡的影响
  • 批准号:
    1304700
  • 财政年份:
    2013
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Standard Grant
Enhanced Spatial Resolution Surface Melting over the Antarctic Peninsula (1958 - to date) from a Regional Climate Model Validated through Remote Sensing Observations
通过遥感观测验证的区域气候模型增强空间分辨率的南极半岛表面融化(1958 年至今)
  • 批准号:
    1141973
  • 财政年份:
    2012
  • 资助金额:
    $ 40.52万
  • 项目类别:
    Continuing Grant

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