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

• 批准号: 1713072
• 负责人: Marco Tedesco
• 金额: $ 40.52万
• 依托单位: Columbia University
• 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
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1713072&HistoricalAwards=false
• 关键词: Collaborative; Research; Closing; Gaps; Climate

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.

表面反照率是衡量介质反射的太阳辐射百分比的指标。反照率越高（越低），介质吸收的太阳能量就越低（越高）。反照率在格陵兰冰盖上起着至关重要的作用，吸收的太阳辐射是夏季表面融化的主要驱动力。格陵兰冰盖反照率的演变主要是由雪粒大小的变化、表面液态水的存在、裸露冰的暴露以及雪和冰中吸光杂质的存在驱动的。 这些杂质包括烟灰、灰尘以及细菌和藻类等生物成分。 生物杂质和雪物理过程（例如变质作用和融化物重新分布）之间的相互作用很重要，因为它们可以驱动正反馈，从而放大总融化量。尽管它们很重要，但这些将生物成分与冰雪演化相关的过程目前在用于模拟格陵兰岛对海平面上升的贡献的当前估计和未来预测的模型中要么不存在，要么很少得到体现。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先进知识整合到气候模型中。这将有助于减少格陵兰岛对海平面上升的贡献的不确定性，也将提高我们对冰盖与大气之间相互作用的理解。我们研究中将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）。实施的模型改进将及时发布以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解决复杂但关键的科学问题。该项目的结果将传达给媒体和公众，从而促进人们更深入地了解影响格陵兰冰盖表面质量平衡的过程。

项目成果

Mapping Ice Algal Blooms in Southwest Greenland From Space

从太空绘制格陵兰岛西南部冰藻繁殖图

• DOI: 10.1029/2018gl080455
• 发表时间: 2018-11-16
• 期刊: Geophysical Research Letters
• 影响因子: 5.2
• 作者: Shujie Wang;M. Tedesco;Min Xu;P. Ale;er;er
• 通讯作者: er

Spectral attenuation coefficients from measurements of light transmission in bare ice on the Greenland Ice Sheet

格陵兰冰原裸冰光透射测量的光谱衰减系数

• DOI: 10.5194/tc-15-1931-2021
• 发表时间: 2021-04-21
• 期刊: The Cryosphere
• 作者: M. Cooper;L. Smith;Å. Rennermalm;M. Tedesco;R. Muthyala;S. Leidman;S. Moustafa;J. Fayne
• 通讯作者: J. Fayne

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: 2021-01
• 期刊: and Alpine Research
• 作者: Scambos, Ted;Straneo, Fiamma;Tedesco, Marco
• 通讯作者: Tedesco, Marco

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: 2019-03
• 期刊: Journal of Geophysical Research: Earth Surface
• 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.

Assessing bare-ice albedo simulated by MAR over the Greenland ice sheet (2000–2021) and implications for meltwater production estimates

评估 MAR 模拟的格陵兰冰盖裸冰反照率（2000 年至 2021 年）及其对融水产量估计的影响

• DOI: 10.5194/tc-16-4185-2022
• 发表时间: 2022-10-11
• 期刊: The Cryosphere
• 作者: R. Antwerpen;M. Tedesco;X. Fettweis;P. Ale;er;er;W. J. van de Berg
• 通讯作者: W. J. van de Berg