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Ground-based radar observations of snow stratigraphy and melt processes in the percolation facies of the Greenland ice sheet

机译：格陵兰冰盖渗透相的雪地层和熔体过程的地基雷达观测

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I.H.H. Zabel; K.C. Jezek; P.A. Baggeroer; S. P. Gogineni;
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年度 1995
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1. A ground-based radar backscatter investigation in the percolation zone of the Greenland ice sheet [J] . Julian B. T. Scott, Doug Mair, Pete Nienow, Remote Sensing of Environment: An Interdisciplinary Journal . 2006,第4期

机译：格陵兰冰原渗流区的地面雷达反向散射调查
2. High-resolution study of layering within the percolation and soaked facies of the Greenland ice sheet [J] . Joel BROWN, Joel HARPER, W. Tad PFEFFER, Annals of Glaciology . 2011,第59期

机译：格陵兰冰盖渗流和浸润相中分层的高分辨率研究
3. Mapping of ice layer extent and snow accumulation in the percolation zone of the Greenland ice sheet [J] . S. V. Nghiem, K. Steffen, G. Neumann, Journal of geophysical research. Earth Surface: JGR . 2005,第f2期

机译：格陵兰冰原渗流区冰层范围和积雪的制图
4. Radar scattering from snow facies of the Greenland ice sheet: results from the AIRSAR 1991 campaign [C] . Rignot, E., Jezek, Geoscience and Remote Sensing Symposium, 1993. IGARSS '93. Better Understanding of Earth Environment., International . 1993

机译：格陵兰冰原雪相的雷达散射：AIRSAR 1991年运动的结果
5. Characterizing the relationship between Ku-band radar backscatter and snow accumulation on the Greenland ice sheet [D] . Miller, Julie 2012

机译：表征格带雷达反向散射与格陵兰冰原上积雪之间的关系
6. Greenland Ice Sheet surface melt amplified by snowline migration and bare ice exposure [O] . J. C. Ryan, L. C. Smith, D. van As, 2019

机译：格陵兰冰原的表面融化因雪线迁移和裸露的冰雪而加剧
7. Spectral and Angular Ground-Based Radar BackScatter Measurements of Greenland Snow Facies. [O] . Baumgartner F, Jezek K, Forster R. R, 2008

机译：格陵兰雪相的光谱和角度地面雷达Backscatter测量。
8. Radar Scattering From Snow Facies of the Greenland Ice Sheet: Results from the AirSar 1991 Campaign [R] . Lou., E. Rignot K. Jezek J. J. Van Zyl M. R. Drinkwater Y. L. 1993

机译：格陵兰冰盖雪相的雷达散射：airsar 1991运动的结果

Ground-based radar observations of snow stratigraphy and melt processes in the percolation facies of the Greenland ice sheet

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