Combined observations of Arctic sea ice with near-coincident colocated X-band, C-band, and L-band SAR satellite remote sensing and helicopter-borne measurements

被引:35
|
作者
Johansson, A. M. [1 ]
King, J. A. [2 ]
Doulgeris, A. P. [1 ]
Gerland, S. [2 ]
Singha, S. [3 ]
Spreen, G. [2 ,4 ]
Busche, T. [5 ]
机构
[1] UiT, Dept Phys & Technol, Tromso, Norway
[2] Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway
[3] German Aerosp Ctr DLR, Remote Sensing Technol Inst IMF, Bremen, Germany
[4] Univ Bremen, Inst Environm Phys, Bremen, Germany
[5] German Aerosp Ctr DLR, Microwaves & Radar Inst HR, Wessling, Germany
关键词
N-ICE2015; remote sensing; sea ice; SYNTHETIC-APERTURE RADAR; FALL FREEZE-UP; SURFACE-ROUGHNESS; FRAM STRAIT; BALTIC SEA; THICKNESS; CLASSIFICATION; SIGNATURES; AIRBORNE; IMAGES;
D O I
10.1002/2016JC012273
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
In this study, we compare colocated near-coincident X-, C-, and L-band fully polarimetry SAR satellite images with helicopter-borne ice thickness measurements acquired during the Norwegian Young sea ICE 2015 (N-ICE2015) expedition in the region of the Arctic Ocean north of Svalbard in April 2015. The air-borne surveys provide near-coincident snow plus ice thickness, surface roughness data, and photographs. This unique data set allows us to investigate how the different frequencies can complement one another for sea ice studies, but also to raise awareness of limitations. X-band and L-band satellite scenes were shown to be a useful complement to the standard SAR frequency for sea ice monitoring (C-band) for lead ice and newly formed sea ice identification. This may be in part be due to the frequency but also the high spatial resolution of these sensors. We found a relatively low correlation between snow plus ice thickness and surface roughness. Therefore, in our dataset ice thickness cannot directly be observed by SAR which has important implications for operational ice charting based on automatic segmentation.
引用
收藏
页码:669 / 691
页数:23
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