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: 1712695
• 负责人: Mark Flanner
• 金额: $ 10.16万
• 依托单位: Regents of the University of Michigan - Ann Arbor
• 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 2022-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1712695&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.

表面反射率是测量被介质反射的太阳辐射的百分比。太阳能吸收率越高（越低），介质吸收的太阳能就越低（越高）。反照率在格陵兰冰盖上起着关键作用，吸收的太阳辐射是夏季表面融化的主要驱动力。格陵兰冰盖上冰的演变主要是由雪颗粒大小的变化、表面液态水的存在、裸露的冰的暴露以及雪和冰中存在的吸光杂质所驱动的。 这些杂质包括烟灰、灰尘和细菌和藻类等生物成分。 生物杂质和雪物理过程之间的相互作用（例如，变质作用和熔体再分布）是重要的，因为它们可以驱动正反馈，其中总熔体被放大。尽管它们的重要性，这些过程有关的生物成分的雪和冰的演变是目前不存在或很少代表的模型用于模拟目前的估计和未来的预测格陵兰岛的贡献，海平面上升。通过跨学科的合作努力，该项目将把生物活动如何影响热带气旋的最新知识纳入气候模型。这将有助于减少格陵兰岛对海平面上升贡献的不确定性，也将提高我们对冰盖和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，地球系统模型（Earth System Model）。实施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研究员的参与，从而培训年轻的研究人员通过跨学科努力解决复杂而关键的科学问题。该项目的成果将向媒体和公众通报，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

SNICAR-ADv4: a physically based radiative transfer model to represent the spectral albedo of glacier ice

SNICAR-ADv4：基于物理的辐射传输模型，用于表示冰川冰的光谱反照率

• DOI: 10.5194/tc-16-1197-2022
• 发表时间: 2022
• 期刊: The Cryosphere
• 作者: Whicker, Chloe A.;Flanner, Mark G.;Dang, Cheng;Zender, Charles S.;Cook, Joseph M.;Gardner, Alex S.
• 通讯作者: Gardner, Alex S.

SNICAR-ADv3: a community tool for modeling spectral snow albedo

• DOI: 10.5194/gmd-14-7673-2021
• 发表时间: 2021-12-21
• 期刊: GEOSCIENTIFIC MODEL DEVELOPMENT
• 影响因子: 5.1
• 作者: Flanner, Mark G.;Arnheim, Julian B.;Zender, Charles S.
• 通讯作者: Zender, Charles S.