500–2000-MHz Brightness Temperature Spectra of the Northwestern Greenland Ice Sheet
500–2000-MHz Brightness Temperature Spectra of the Northwestern Greenland Ice Sheet
复制标题
格陵兰岛西北部冰盖的 500–2000 MHz 亮度温度光谱
DOI:
10.1109/tgrs.2017.2764381
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发表时间:
2018
影响因子:
8.2
通讯作者:
M. Aksoy
中科院分区:
文献类型:
--
作者:
K. Jezek;J. Johnson;Shurun Tan;L. Tsang;M. Andrews;M. Brogioni;G. Macelloni;M. Durand;Chi;Domenic J. Belgiovane;Yuna Duan;C. Yardim;Hongkun Li;A. Bringer;V. Leuski;M. Aksoy
An ultra-wideband radiometer has been developed to measure subsurface properties of the cryosphere including ice sheets and sea ice. The radiometer measures brightness temperature spectra from 0.5 to 2 GHz using 12 channels, each of which measures scene brightness temperatures over an ~88-MHz bandwidth resolved into 0.24-MHz intervals. The instrument was flown over northwestern Greenland in September 2016 and acquired the first, wideband, low-frequency brightness temperature spectra over the ice sheet and coastal region. The results reveal strong spatial and spectral variations that correlate well with the physical properties of the surface encountered along the flight path, which started over ocean, then passed the rock near the coast, and then up onto the ablation, wet, percolation, and dry snow zones of the interior ice sheet. In particular, strong spectral responses in percolation and dry snow zones are observed and plausibly explained by varying the distribution of horizontal density layers and isolated icy bodies in the upper portion of the firn. The success of the airborne deployment of the instrument and subsequent implementation of algorithms to limit radio frequency interference in unprotected bands is motivating continued airborne investigations as well as stimulating research into the feasibility of a spaceborne instrument.