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Collaborative Research: Deciphering the Deep Ice and the Ice-water Interface over Lake Vostok Using Existing Radar Data

Collaborative Research: Deciphering the Deep Ice and the Ice-water Interface over Lake Vostok Using Existing Radar Data
合作研究:利用现有雷达数据破译沃斯托克湖上的深冰和冰水界面
批准号:
0538674
负责人:
Dale Winebrenner
金额:
$0.0万
依托单位:
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2006
资助国家:
美国
项目状态:
已结题
起止时间:
2006-04-01 至 2011-03-31

项目摘要

项目成果

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中文摘要
翻译
0538674松冈该奖项支持一个项目,评估覆盖沃斯托克湖的网格上可用的穿冰雷达数据中的无线电回波强度,以及从B岭到该湖的四条区域轨道。该项目有两个目标;首先,它将检查湖面和反射器,这些反射器被假设为陨石和凝结冰之间的边界。他们将提供有关该湖动态演变的关键知识。其次,该项目将研究东南极洲中部深层冰层中一个知之甚少的无回声区域。这一带可能由变形的死冰组成,而其上边界可能是剪切带。SOAR雷达数据为研究时空水循环模式提供了独特的资源,应当了解这些模式,以便选择对湖泊进行最佳直接采样的策略。Vostok冰芯为这项工作提供了一个独特的机会。首先,路径效应,即传播损耗和双折射,将在冰芯位置使用冰温、化学和组构数据进行推导。其次,传播损失的横向变化将通过跟踪与雷达探测到的等时层相关的化学物质,并通过从可以复制这些层的冰流模型推断温度来估计。将从大约100个雷达航迹交叉点的反射率各向异性中推断出冰的结构模式。在更广泛的影响方面,将培训一名研究生根据雷达理论和沃斯托克湖的冰川学背景解释雷达数据,并将在西雅图和纽约为K-12教师举办暑期讲习班。该项目将有助于正在进行的研究沃斯托克湖的努力,并将补充俄罗斯和法国作为国际海洋年计划提出的北沃斯托克冰芯的选址。
英文摘要
0538674MatsuokaThis award supports a project to evaluate radio-echo intensities in the available SOAR ice-penetrating radar data along grids covering Lake Vostok, and along four regional tracks from Ridge B toward the lake. The project has two objectives; first, it will examine the upper surface of the lake and reflectors hypothesized to be a boundary between the meteoric and accreted ice. They will provide crucial knowledge on the dynamic evolution of the lake. Second, this project will examine a poorly understood echo-free zone within the deep ice in central East Antarctica. This zone may consist of distorted stagnant ice, while its upper boundary may be a shear zone. The SOAR radar data provide a unique resource to examine spatiotemporal water circulation patterns that should be understood in order to select the best direct-sampling strategy to the lake. The Vostok ice core provides a unique opportunity to do this work. First, the path effects, i.e. propagation loss and birefringence, will be derived at the ice-core site using ice temperature, chemistry, and fabric data. Second, lateral variations of the propagation loss will be estimated by tracking chemistry associated with radar-detected isochronous layers, and by inferring temperatures from an ice-flow model that can replicate those layers. Ice-fabric patterns will be inferred from anisotropy in the reflectivity at about 100 radar-track cross-over sites. In terms of broader impacts, a graduate student will be trained to interpret the radar data in the light of radar theory and glaciological context of Lake Vostok and summer workshops for K-12 teachers will be provided in Seattle and New York. This project will contribute to ongoing efforts to study Lake Vostok and will complement the site selection for a North Vostok ice core, which has been proposed by Russia and France as an IPY program.
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